آمار و اطلاعات

 آمار و اطلاعات 

آّشنایی با جزر و مد (Tides)

منبع : حمل و نقل دریایی

آّشنایی با جزر و مد (Tides)

Tides

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Tidal movements

The tide is the vertical rise and fall of the sea level surface caused primarily by the change in gravitational attraction of the moon, and to a lesser extent the sun.
As the earth spins on its axis the centrifugal force results in slightly deeper water near the equator as opposed to shallower water at the poles. In fact it causes a flow from the poles to the equator.
The earth is also in orbit around the sun (one revolution in one year) creating not only another centrifugal force but also a gravitational interaction. These two yield a bulge on the night site (centrifugal) and a bulge on the day site (gravitational) both of them moving as the world turns. Therefore, a certain place on this world will experience two high and two low tides each day.
With these forces alone, we would not have spring tides and neap tides. Spring tides have higher high tides and lower low tides whereas neap tides have lower high tides and higher low tides. Hence, the range (difference in water level between high and low tide) is much larger in a spring tide than in a low tide.

This animation shows how the tide changes during the lunar cycle. When the sun, moon and earth are aligned : spring tide.
When at right angles the forces are not aligned:
neap tide.
The time between spring and neap is approximately 7 days.

These differences in range can be explained if we include the moon into our earth-sun system. The moon and the earth orbit each other around a point (called the barycenter or baricenter) 2000 odd kilometres inside the earth, creating a centrifugal and a gravitational bulge. Moreover, despite the sun's immensely larger mass, the moon exerts a 2.25 times larger gravi­tatio­nal attraction, since the moon is much closer to our earth.
It is the combined effect of the sun and moon that creates spring and neap tides. In the animation the gravitational forces of both the sun and the moon are taken into account. When aligned with the earth they combine their attraction and otherwise they counteract their attraction. The sun is located in the corner right below, far outside this picture (note the eclipse) while the moon is revolving round the earth. One full circle corresponds to one lunar cycle (about 28 days).

The figure below shows the ideal sinusoids of both spring and neap tides. Vertically the water height is shown versus horizontally the time. Ideally, the time between a low and a successive high is somewhat more than 6 hours.
The sinoidal 
curve of the Tide
The time difference between spring tide and neap tide is normally 7 days and is in accordance with the phases of the moon. Yet, water has mass and therefore momentum. Moreover, it is a viscous fluid that generates friction if moved. Therefore, the actual spring tide lags a day or so behind a full moon or new moon occurrence.

So, tidal movements are intrinsically periodical, resulting in a Tidal day of 24 hours and 50 minutes containing one tidal cycle, namely two highs and two lows. This basic pattern may be distorted by the effects of landmasses, constrained waterways, friction, the Coriolis effect, or other factors. Hence, predictions are possible and we expect the the next day's high tide to come about 50 minutes later.
However, a closer look at the orbit of the moon reveals that the moon is not always in the equatorial plane, resulting in three types of tides:

Semi-diurnal tide: Featuring two highs and two lows each day, with minimal variation in the height of successive high or low waters. This type is more likely to occur when the moon is over the equator.

Diurnal tide: Only a single high and a single low during each tidal day; successive high and low waters do not vary by a great deal. This tends to occur in certain areas when the moon is at its furthest from the equator.

Mixed tide: Characterized by wide variations in heights of successive high and low waters, and by longer tidal cycles than those of the semi-diurnal cycle. These tides also tend to occur as the moon moves furthest north or south of the equator.

Chart Datums

The depths and heights in the chart need a plane of reference: the Chart Datum (see interactive figure below). Depths are usually described with respect to low water reference planes (yielding lower charted depths, which are safer) and heights are shown with respect to high water reference planes (again, yielding lower vertical clearances on the chart, which are safer). As such, the chance that the observed depth or vertical clearance beneath a bridge is smaller than the charted depth or height is rather small.

In this example the Charted Depths are related to LAT.
The Observed Depth or Drying Height is a combination of Tidal Height & Charted Depth.
  This example shows the various spring and neap tides around mean water level. Note that spring low water is the lowest. Both ranges are indicated.   In this example the light elevation is reduced to high water. Also a clearance under a bridge is charted in that way. The 'height' refers to the building itself. On land yet another CD can be in use.


Some Chart Datums and their abbreviations:

MHWS : Mean High Water Spring

HW : High Water

MHWN : Mean High Water Neap

ML : Mean Level

MLWN : Mean Low Water Neap

MLWS : Mean Low Water Spring

LAT : Low Astronomical Tide

 

Overview

Tide: The vertical rise and fall of the surface of a body of water caused primarily by the differences in gravitational attraction of the moon, and to a lesser extent the sun, upon different parts of the earth when the positions of the moon and sun change with respect to the earth.

Spring Tide: The tidal effect of the sun and the moon acting in concert twice a month, when the sun, earth and moon are all in a straight line (full moon or new moon). The range of tide is larger than average.

Neap Tide: This opposite effect occurs when the moon is at right angles to the earth-sun line (first or last quarter). The range of tide is smaller than average.

Range: The vertical difference between the high and low tide water levels during one tidal cycle.

Tidal Day: 24 hours and 50 minutes. The moon orbits the earth every month, and the earth rotates (in the same direction as the moon's orbit) on its axis once every 24 hours.

Tidal Cycle: One high tide plus a successive low tide.

Semi-diurnal Tide: The most common tidal pattern, featuring two highs and two lows each day, with minimal variation in the height of successive high or low waters.

Diurnal Tide: Only a single high and a single low during each tidal day; successive high and low waters do not vary by a great deal. Such tides occur, for example, in the Gulf of Mexico, Java Sea and in the Tonkin Gulf.

Mixed Tide: Characterized by wide variation in heights of successive high and low waters, and by longer tide cycles than those of the semidiurnal cycle. Such tides occur, for example, in the U.S. Pacific coast and many Pacific islands.

Chart Datum or Tidal reference planes: These fictitious planes are used as the sounding datum for the tidal heights.

Drying Height: Clearance in meters (or feet in old charts) above the chart datum.

Charted Depth: Clearance in meters (or feet in old charts) below the chart datum.

Observed Depth: Height of tide + charted depth: the actual depth in meters.

Height of light: The height of light above the bottom of its structure.

Elevation: The height of the light above the chart datum.

Rule of Twelve: Assuming a tidal curve to be a perfect sinusoid with a period of 12 hours. The height changes over the full range in the six hours between HW and LW with the following fractions during each respective hour: 1/12  2/12  3/12  3/12  2/12  1/12.

Rule of Seven: The change from spring range to neap range can be assumed linear, each day the range changes with 1/7th of difference between the spring and neap ranges. Hence, the daily change in range = (spring range - neap range)/7.

Tides & tidal
prediction

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1 - Information from the chart

Position of tabulated tidal levels data with designation 'a' - 
chart symbol Most often the chart presents succinct tide tables for certain positions. These positions are marked with the “square”. The table below shows us an example for two different positions. The first refers to Cowes (UK), the second to a position south of Cowes.

 Position Heights above LAT
Mean HW Mean LW
Spring Neap Spring Neap
 Cowes 1,7 m 1,5 m 0,2 m 0,4 m
Position of tabulated tidal levels data with designation 'a' - 
chart symbol 5,2 m 4,3 m 0,4 m 1,2 m

This data only provides us with average high and low waters heights. Moreover, it is merely valid at spring or neap tides. To use it we need to first find out how many hours we are from high water. Secondly, we need to know if it is spring or neap or sometime in between at that particular moment. We shall use this table to solve two types of problems. Finding height of tide at a particular location at a particular time:

To get over a shoal.

To pass under a bridge.

Almanacs and many other nautical publications contain predictions of the times of high and low tides at many major standard ports. Also listed are differences in times of tides from these ports for additional secondary ports. To work with this succinct data we need two extra tools:

Rule of
 twelve To interpolate between high and low water heights we use the Rule of Twelve. We assume the tidal curve to be a perfect sinusoid with a period of 12 hours. The height changes over the full range in the six hours between HW and LW.

  • During first hour after heigh water (HW) the water drops 1/12th of the full range.
  • During the second hour an additional 2/12th.
  • During the third hour an additional 3/12th.
  • During the fourth hour an additional 3/12th.
  • During the fifth hour an additional 2/12th.
  • During the sixth hour an additional 1/12th.

Hence, two hours after the HW the water has fallen 3/12 of the full range.

To interpolate between spring and neap tides we use the Rule of Seven. Since the change from spring range to neap range can be assumed linear (instead of sinusoid), each day the range changes with 1/7th of difference between the spring and neap ranges.
Hence, the daily change in range is (spring range - neap range)/7.

Shoal problem:
Our shoal near Cowes has a charted depth of 1 meter and we would like to cross it at about 15:00 hours with our yacht (draft 1,5 m).

From any nautical almanac we find that HW occurs at 03:18 15:53 and LW occurs at 09:45 22:03 at a standard port nearby. We also find that at our location HW occurs one hour later and that spring tide is due in two days. Hence, we have a HW around 17:00.

Via the rule of seven we find out that today the range is:
spring range - 2 x ( (spring range - neap range)/7 )
<=> 4,8 - 2 x ( ( 4,8 - 3,1)/7 ) <=> 4,8 - 2 x 0,25 = 4,3 m.

We also need today's HW height:
which is Spring HW - 2 days x ( (5,2 -4,3)/7 ) = 5,0 m.

Via the rule of twelve we find out that at two hours before high water the height is:
5,0 - 3/12 x 4,3 = height at 15:00 hours = 3,9 m.

So, after three interpolations we derive the water height at 1500 hours. Considering the charted depth leads to an observed depth of 4,9 meters, enough for our draft of 1,5 meters.

Bridge problem:
An overhanging rock, power lines or bridges have their clearances charted with respect to another chart datum than LAT. Normally, 'high water' or 'MHW spring' are used as reference planes.

An example:
Above our shoal hangs the 'Cowes bridge'. At 15:00 hours we would like to pass this bridge, which has a charted height of 20 meters to HW. Our mast is 23 meters high. In the example above we found that the water height was 1,1 meters below HW level at that time. Obviously, we will have to wait!
So, at what time will we be able to pass under this bridge?
The water height must be 3 meters lower than HW level (5,0 m). That is almost 9/12 of the range (4,3 m) indicating four hours after HW. Conclusion, we will have to wait at least six hours in total.

2 - Information from tide tables

Instead of mere averages, a tide tableDetailed Tide 
Table. provides us each day with the times of high and low water for a particular place. Basically, it is same table like the one we found in the chart, but is extended for every day in a year. By using this method we get more accurate water heights since it involves less interpolation. The example shows us a part of a very detailed tide table, which even includes heights for every hour.

3 - Information from tidal curves

In most tables the tides can also be characterized by a tidal curve. This method substitutes the rule of twelve providing more accurate heights. The left side contains the water height information with the lowest heights to the left where also the chart datum is indicated. The low water height will be marked at the bottom and the high water height will be marked at the top.
Tidal Curve.
The area under the curve will be marked with the time information.
To find the water height at a specific time we need to know first how many hours before or after the HW this is. Then

Tidal Curve:

Finding Heights.

Tidal Curve:

Finding Time with Height.
Often this is done when the curve is not sinusoid and the rule of twelve is rendered useless.

 

Overview

Tide: The vertical rise and fall of the surface of a body of water caused primarily by the differences in gravitational attraction of the moon, and to a lesser extent the sun, upon different parts of the earth when the positions of the moon and sun change with respect to the earth.

Spring Tide: The tidal effect of the sun and the moon acting in concert twice a month, when the sun, earth and moon are all in a straight line (full moon or new moon). The range of tide is larger than average.

Neap Tide: This opposite effect occurs when the moon is at right angles to the earth-sun line (first or last quarter). The range of tide is smaller than average.

Range: The vertical difference between the high and low tide water levels during one tidal cycle.

Tidal Day: 24 hours and 50 minutes. The moon orbits the earth once earth month, and the earth rotates (in the same direction as the moon's orbit) on its axis once every 24 hours.

Tidal Cycle: A successive high and low tide.

Semi-diurnal Tide: The most common tidal pattern, featuring two highs and two lows each day, with minimal variation in the height of successive high or low waters.

Diurnal Tide: Only a single high and a single low during each tidal day; successive high and low waters do not vary by a great deal. Gulf of Mexico, Java Sea and in the Tonkin Gulf.

Mixed Tide: Characterized by wide variation in heights of successive high and low waters, and by longer tide cycles than those of the semidiurnal cycle. U.S. Pacific coast and many Pacific islands.

Chart Datum or Tidal reference planes: These fictitious planes are used as the sounding datum for the tidal heights.

Drying Height: Clearance in meters (or feet in old charts) above the chart datum.

Charted Depth: Clearance in meters (or feet in old charts) below the chart datum.

Observed Depth: Height of tide + charted depth: the actual depth in meters.

Height of light: The height of light above the bottom of its structure.

Elevation: The height of the light above the chart datum.

Rule of Twelve: Assuming a tidal curve to be a perfect sinusoid with a period of 12 hours. The height changes over the full range in the six hours between HW and LW with the following fractions during each respective hour: 1/12  2/12  3/12  3/12  2/12  1/12.

Rule of Seven: The change from spring range to neap range can be assumed linear, each day the range changes with 1/7th of difference between the spring and neap ranges. Hence, the daily change in range = (spring range - neap range)/7.



مقایسه آماری از حجم تخلیه و بارگیری کالا در دنیا با استفاده از ناوگان دریا

منبع : حمل و نقل دریایی

مقایسه آماری از حجم تخلیه و بارگیری کالا در دنیا با استفاده از ناوگان دریا

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سايت سازمان بنادر ودريانوردي ايران

(international maritime organization)

www.pmo.ir

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کار عملی با نقشه های دریایی

منبع : حمل و نقل دریایی

کار عملی با نقشه های دریایی

Plotting and piloting

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Lines of position

The modern chart shows us positions of many recognizable aids to navigation like churches and lighthouses, which facilitate the approach to a coastal area. This concept originated from a chart by Waghenaer and proved a milestone in the development of European cartography. This work was called “Spieghel der Zeevaerdt” and included coastal profiles and tidal information much like the modern chart. It enables us to find the angle between the North and for example an offshore platform, as seen from our position.

Navigation - bearings - LOP
        Compass courses
Compass 
Bearing on Rig = 44 Use Ship's Compass Heading to get Deviation. LOP = 
50.
True courses                        

Taking a bearing on this oil rig with a compass provides us with a compass course. This course first needs correction for both variation and - via ship's heading - deviation before plotting a Line of Position (LOP) in the chart as a true course.
Our position is somewhere along this line.

Ranges

A precise way to obtain a LOP, and without a compass, is to locate two aids to navigation in line. The map of Laura Island on the right shows four examples of ranges, each consisting of two aids to navigation.

Please, note that:

More distance between the two landmarks enhances accuracy.

And less distance between the vessel and the closest aid to navigation also enhances accuracy.

One of these four ranges consists of two lights that are intentionally placed to provide a LOP. These pairs of lights are called range lights or leading lights. In this case they indicate the approach towards the marina and mark the channel between the dangerous rocks along a true course of 50°. When looking towards any leading lights, the nearest one will be lower. A range 
without man-made structures Therefore, in the middle of the channel both lights will appear vertically above each other.

Even when there are no man-made structures available, a range can be found by using natural features such as coastlines and islets. The example on the left shows a yacht that will avoid the dangerous wreck as long as the islets don't overlap.
 

Position fix

If two LOPs intersect we can construct a position fix: the ship's position on the earth.
Often however, a triangle occurs when a third LOP is added in the construction. This indicates that there are errors involved in at least one of the bearings taken. In practice, we should consider each LOP as the average bearing in a wider sector of for instance 10°.

The optimum angular spread is 90° (two objects) or 120° (three objects). Moreover, bearings on distant objects bring about more uncertainty in our position fix as the sector widens. Finally, if moving fast you should not put any time between the bearings.

The next example features a nocturnal landfall on Willemsen Island - you are welcome to visit, but mind the rocks. The position fix is plotted by taking bearings at two light-vessels as their lights appear over the horizon. The variation is -1° and the ship's compass heading is 190°. Since we use our steering compass for our bearings, we can use the same deviation table. That means a deviation of -4° with which we can calculate (cc + var + dev = tc) the true courses.

Construction
Cross bearing
  • Compass bearing on Will. N is 72°
  • True course is 67°
  • Plot LOP with time & true course
    Cross bearing
  • Compass bearing on Will. S is 173°
  • True course is 168°
  • Plot LOP with time & true course
    Cross bearing
  • Draw an ellipse where the LOPs intersect
  • Notate time and “Fix” alongside
  • Position is 32° 04,2' N , 24° 46,7' E
Sailing schools in Athens Navigation chart, coordinates

Without a third LOP - forming the dreaded triangle - there is the false suggestion of accuracy. Yet, instrument errors, erroneous identification of an aid to navigation, sloppy plotting, etc. can and will cause navigation errors. Therefore, if close to e.g. rocks, you should assume to be at the worst possible position (i.e. closest to the navigational hazard).

The lines plotted in the chart are always true courses and these are labeled with true courses by default; the “T” is optional. If labeled with the corresponding magnetic course or compass course add an “M” or “C”, respectively.

Estimated position

It is sometimes impossible to obtain more than one LOP at a time. To determine the ship's position with one aid to navigation we can use a running fix. However if a running fix is not possible, we can determine an estimated position.

Estimated position plot : One LOP plus DR position gives EP. An estimated position is based upon whatever incomplete navigational information is available, such as a single LOP, a series of depth measurements correlated to charted depths, or a visual observation of the surroundings.

In the example on the right we see an estimated position constructed using a single LOP and the ship's dead reckoning position (DR). This is done by drawing a line from the DR position at the time of the LOP perpendicular to the LOP. An EP is denoted by a square instead of an ellipse.

Do not rely on an EP as much as a fix. The scale of reliability, from best to worst:

Fix

Running fix

Estimated position

DR position

Dead reckoning

Dead reckoning is a technique to determine a ship's approximate position by applying to the last established charted position a vector or series of vectors representing true courses and speed. This means that if we have an earlier fix, we plot from that position our course and “distance travelled since then” and deduce our current position.

09:30 We start off with a Fix and plot a DR position for 15 minutes later.
09:45 Our estimation about our speed and course was correct, so we don't have to charge the DR position.
10:00 and so on…
S = Speed through water (not over ground)
C = Course through water (not over ground)
       T = True course (default)
       M = Magnetic course for handheld compass (no deviation correction)
       C = Compass course for steering compass (deviation correction)
Mark with an arrow, a semi-circle (circular arc) and “DR”.
  Dead reckoning

Dead reckoning is crucial since it provides an approximate position in the future. Each time a fix or running fix is plotted, a vector representing the ordered course and speed originate from it. The direction of this course line represents the ship's course, and the length represents the distance one would expect the ship to travel in a given time. This extrapolation is used as a safety precaution: a predicted DR position that will place the ship in water 1 metre deep should raise an eyebrow…
In the example above the true courses are plotted in the chart, and to assist the helmsman these course lines are labelled with the corresponding compass courses.
Guidelines for dead reckoning:

Plot a new course line from each new fix or running fix (single LOP).

Never draw a new course line from an EP.

Plot a DR position every time course or speed changes.

Plot a corrected DR position if the predicted course line proofed wrong, and continue from there.

Running fix

Under some circumstances, such as low visibility, only one line of position can be obtained at a time. In this event, a line of position obtained at an earlier time may be advanced to the time of the later LOP. These two LOPs should not be parallel to each other; remember that the optimal angular spread is 90°. The position obtained is termed a running fix because the ship has “run” a certain distance during the time interval between the two LOPs.

09:16 We obtain a single LOP on LANBY 1 and plot a corresponding (same time) dead reckoning position. The estimated position is constructed by drawing the shortest line between the DR and the LOP: perpendicular.
09:26 No LOPs at all. We tack and plot a DR position.
09:34 We obtain a LOP on LANBY 2. To use the first LOP we advance it over a construction line between the two corresponding DR positions. We use both its direction & distance.
  Running fix

To use the LOP obtained at an earlier time, we must advance it to the time of the second LOP. This is done by using the dead reckoning plot. First, we measure the distance between the two DR positions and draw a construction line, which is parallel to a line connecting the two DR positions.
Note that if there are no intervening course changes between the two DR positions, it's easiest just to use the course line itself as the construction line.
Now, using the parallel rulers we advance the first LOP along this construction line over the distance we measured. Et voilá, the intersection is our RFix.
If there is an intervening course change, it appears to make our problem harder. Not so! The only DR positions that matter are the two corresponding with the LOPs.
Guidelines for advancing a LOP:

The distance: equal to the distance between the two corresponding DR positions.

The direction: equal to the direction between the two corresponding DR positions.

Draw the advanced LOP with a dotted line and mark with both times.

Label the Running Fix with an ellipse and "RFix" without underlining.

Danger bearing

Like the dead reckoning positioning, the danger bearing is an important tool to keep the ship out of harm's way.Danger 
bearings are plotted in advance 

to sail clear from danger. First, the navigator identifies the limits of safe, navigable water and determines a bearing to for instance a major light. This bearing is marked as “No More Than” (NMT) or “No Less Than” (NLT), depending on which side is safe. Hatching is included on the side that is hazardous, along with its compass bearing.

In the example on the right a true course of 325° is plotted (5° variation), marked with the magnetic course of 320°, practical for a handheld compass that requires no deviation correction.
Were we see that light at 350° magnetic - which is definitely “More Than” - the rocks and wreck would be between us and the major light. A possible cause could be a (tidal) stream from east to west.

When a distance is used instead of a direction, a danger range is plotted much the same way as the danger bearing.

Turn bearing

The Turn bearing - like the danger bearing - is constructed in the chart in advance. It should be used as a means of anticipation for sailing out of safe waters (again like the danger bearing and dead reckoning). The turn bearing is taken on an appropriate aid to navigation and is marked “TB”. As you pass the object its bearing will slowly change. When it reaches the turn bearing turn the vessel on her new course.
This type of bearing is also used for selecting an anchorage position or diving position.

Snellius construction

Willebrord Snellius - a 16th century mathematician from Leiden, the Netherlands - became famous for inventing the loxodrome and his method of triangulation.
The Snellius construction was first used to obtain the length of the meridian by measuring the distance between two Dutch cities. He took angles from and to church towers of villages in between to reach his objective. Nowadays we use the Snellius method to derive our position from three bearings without the use of LOPs, and while leaving out deviation and variation, which simplifies things. Also, since only relative angles are needed a sextant can be used to measure navigation aids at greater distances. Closer in a compass can be used.
The construction:

See figure 1: Compass bearings are 320° on A;   360° on B;   050° on object C.

The angle between A and B = 40°.

The angle between B and C = 50°.

Draw lines from A to B and from B to C.

Add the two light-blue perpendicular bisectors of lines AB and BC.

Draw at object A a construction line 40° inland of line AB.

Draw at object C a second construction line 50° inland of line CB.


First steps of Snellius construction.

See figure 2: At object A: draw a line perpendicular to the construction line.

At object C: draw another line perpendicular to the construction line.

The two intersections with the light-blue lines indicate the centres of two circles.

Finally, draw the first circle using A and B and the second circle using B and C.

The off shore intersection of the two circle gives us our position fix.


Final Snellius construction.

The advantage: deviation and variation can be left out since the angles (here 40° and 50°) are relative ones. Moreover, a sextant can be used to obtain angles between objects at greater distances, that with a compass would be less precise.

International notation

International notation conventions for plotting in the chart
Fix Fix       LOP LOP
Running Fix Running Fix LOP advanced LOP advanced
Estimated Position Estimated Position Course & Speed Course and Speed
Dead Reckoning Dead Reckoning Set & Drift Set and Drift
Electronic Fix (GPS) GPS 
fix    
Electronic Fix (Radar) Radar fix    

Note, that a few countries use an alternative symbol Alternative Fix Symbol

Plotting should be done with a soft pencil. Moreover, avoid drawing lines through the chart symbols. This is to prevent damage to the chart when you have to erase the construction.

Learn sailing and navigation via yacht charters with instruction in Greece.

Glossary

Line Of Position (LOP): The locus of points along which a ship's position must lie. A minimum of two LOPs are necessary to establish a fix. It is standard practice to use at least three LOPs when obtaining a fix, to guard against the possibility of and, in some cases, remove ambiguity.

Transit fix: The method of lining up charted objects to obtain an LOP.

Leading lights or Range lights: A pair of lights or day marks deliberately placed to mark a narrow channel.

Position fix: The intersection of various LOPs.

Cross bearing: The use of LOPs of several navigational aids to obtain a position fix. Remember to use an optimal angular spread.

Running fix: The use of an advanced LOP. Make sure to use only the corresponding DR positions. Also don't use the EP for advancing the first LOP.

Dead reckoning: Determining a position by plotting courses and speeds from a known position. It is also used to predict when lights become visible or to determine the set and rate of a current.

Estimated position: Combine a corresponding DR position with a single LOP to get an EP position.

Snellius construction: Another way to combine three compass bearings to obtain a position fix. The advantage over a cross bearing is that both magnetic variation and deviation don't need to be taken into account.

Course: (C) The direction in which a vessel is steered or is intended to be steered (direction through the water). Course to steer: Course to steer to counteract current and leeway [bovenstroomse koers].
Heading (HDG): The direction in which the boat is pointing in any instant [voorliggende koers].
Course To Make Good (CTMG): The course for planning purposes that indicates the intended track from departure to destination.

Course Made Good (CMG): The single resultant direction from the point of departure to the point of arrival at any given time. Course line Construction line Danger range -->

Speed: (S) The speed of the boat through the water. Speed Made Good (SMG): The speed of the boat achieved over the CMG line.
-->

Set: (SET) The direction in which the current is flowing (see chapters 6,7 and 8).

Drift: (DFT) The speed (in knots) of the current (see chapters 6,7 and 8).

Default heading is True course (M = magnetic , C = compass).

Default time is 24 hour clock ship time else UTC.

Piloting and
navigation

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Doubled angle fix

The Doubled angle on the bow fix resembles a running fix though only one navigation aid is used.

double angle
 on the bow fix
α = 30° , β = 60°
δ = 120° , γ = 30°
Isosceles    d1 = d2

In the example on the right the initial angle (30°) on the bow is doubled (60°) yielding an isosceles triangle. The distance travelled between the bearings is the same as the distance from the visible wreck.

Start with the visible wreck having a bearing of less than 45° off the bow (α), note the log distance.

Proceed along the course until the angle on the bow is doubled (β), read the log: d1 is 10 nm.

Use the log distance to find the position on the second LOP. It is an isosceles triangle, so d2 is also 10 nm.

Label it with an ellipse and "RFix" but realize it is less precise than a running fix that involves two navigation aids.



 

Four point fix

If the first angle on the bow is 45°, a special situation occurs: The Four point fix, so called since 45 degrees equals 4 points on the compass (1 point = 11,25°).

four 
point fix
α = 45° , β = 90°
δ = 90° , γ = 45°
Isosceles    d1 = d2

Start with a bearing with 45° on the bow (α), note the log.

Proceed along the course till the angle on the bow is 90° (β), read the log: d1 is 4 nm

Use the log distance to find the position on the second LOP. Isosceles, so d2 is also 4 nm.

Label it with an ellipse and "RFix".



 

Special angle fix

The Special angle fix requires the mariner to know some special pairs of angles (a : b) that give the distance travelled between bearings as equal to the distance abeam.

special angle fix
α = 21° , β = 32°
d1 = d2

In the example on the right α = 21° and β = 32° are used. Now, the log distance equals the shortest distance between wreck and course line (6 nm).
A few practical pairs:

16 : 22      21 : 32
25 : 41      32 : 59
37 : 72      40 : 79


Remember: the greater the angular spread the better. Hence, of these three fixes the four point fix is the most precise one.

Enter α (1-45°):
β:

Mathematics: isosceles triangle fixes

Distance of the horizon

On a flat world there would be no difference between the visible and sensible horizon. However, on Earth the visible horizon appears several arc minutes below the sensible horizon due to two opposing effects: Horizon with 
atmospherical refraction and 

the curvature of the earth's surface.

the curvature of the earth's surface;

atmospheric refraction.

Atmospheric refrac­tion bends light rays pas­sing along the earth's sur­face to­ward the earth. There­fore, the geo­metr­ical hori­zon ap­pears ele­vated, for­ming the vi­sible ho­rizon.
The distance of the visible horizon is a (semi-empirical) function of Eye Height:

Distance of vis. horizon (nm) 

with height of eye in metres. 



This is a simplified function. 


 

Mathematics: horizon distances

 

 

Dipping range

If an object is observed to be just rising above or just dipping below the visible horizon, its distance can be readily calculated using a simple formula. 365 kb The object's elevation (the height of a light above chart datum) can be found in the chart or other nautical publication such as the 'List of Lights'. Note that in some charts elevation is referred to a different datum than soundings. Click on the image on the right to view a magnificent lighthouse.

Dipping 
distance

The formula contains the two distances from the visible horizon and can be simplified by the equation: 2.08 x (√Elevation + √Eye height). Many nautical publications contain a table called "distances of the horizon" which can be used instead of the equation.
Use the dipping range to plot a Distance LOP in the chart: a circle equal in radius to the measured distance, which is plotted about the navigation aid. Finally, take a bearing on the object to get a second LOP and a position fix.

Enter Eye height (metres):
Enter Elevation (metres):

Distance is (nm):


 

Vertical sextant angle

Similarly, a distance LOP can be obtained by using a sextant to measure the angle (arc) between for instance the light and chart datum of a lighthouse or any other structure of known elevation. Once the angle is corrected for index error the distance can be found in a table called: "Distances by Vertical Sextant Angle", which is based on the following equation.

Vertical 
sextant angle...        Looking through sextant.

Range 
in nm. 

Elevation in metres 

Water Height in metres 

Angle in minutes total.


 

The angle in minutes total, thus 1° 12' = 72' total, and corrected for index error.

Elevation in metres.

Water height in metres above or below chart datum of object.

Distance or Range in nautical miles.

Ascertain whether the base of the object is beyond the horizon

Corrected angle should be greater than 20'.

Though tables can be used for quick reference, this function is valid for objects higher than usually tabulated. An example with a lighthouse of 80 metres:

Measured angle is 1° 19', index error is +6': angle = 73'.

Let's assume water height at 3 metres above Mean Level datum.

Range = 1.854*(80-3/73) = 1.96 nm.

The range can be used as a danger bearing.
Together with a compass bearing one object with known elevation results in a position fix. If more than one vertical sextant angle is combined the optimum angular spread should be maintained.

Enter Angle (minutes total):
Enter Elevation (metres):

Distance is (nm):


Often, the correction for water height can be left out. Though, realizing that the horizon is closer than one might think, another correction is sometimes needed. In the Mediterranean Sea for example we can see mountain tops with bases lying well beyond the horizon. Mutatis mutandis, the structures, which they bear have bases beyond the horizon as well.

Angle over 
horizon...        Looking through sextant.

Range 
in nm. 

Elevation in metres 

Angle in minutes total

Eye Height in metres.

This is the equation for finding the distance of an object of known elevation located beyond the horizon. In the denominator of this equation a compensating factor is included by which the measured angle should be reduced.

Enter Eye Height (metres):
Enter Angle (minutes total):
Enter Elevation (metres):

Distance is (nm):


 

Mathematics: vertical sextant angles

 


 

Estimation of distance

The most obvious way to estimate distances is of course by using the distance between our eyes. There is NO
 part of the author in this image !!!!!!! If we sight over our thumb first with one eye then with the other, the thumb moves across the background, perhaps first crossing a tower second crossing a bridge.

The chart might tell that these structures are 300 m apart.
Use the ratio of: distance between eye and outstretched arm/distance between pupils: usually 10.
The objects are 3 kilometres away.
Other physical relationships are useful for quick reference. For example, one finger width held at arm's length covers about 2° arc, measured horizontally or vertically.
Two fingers cover 4°. Three fingers cover 6° and give rise to the three finger rule:
"An object that is three fingers high is about 10 times as far away as it is high."
 

Estimation with horizon

The image on the right shows us that it is possible to estimate the height of any object that crosses the horizon as seen from our own point of view.

The 
height of the rock equals your height 

since the top aligns with the horizon.

This picture of the 'Pigeon Rocks' near Beirut harbour was taken from a crow's nest at a height of 34 metres.
The distance of the visible horizon (12 nm) is far larger than 34 metres. Therefore, we can - without any other information - estimate that these rocks have a height of 34 metres as well.

Factum: All tops crossing the horizon and with bases at sea level are on eye level.

Furthermore, if we see these rocks over a vertical angle of for example 7° = 0.1225 rad., then the range is 34/0.1225 = 277 metres.
Finally, plot both range and bearing in the chart to construct an EP, et Voilà!

Fix by depth soundings

A series of depth soundings - in this example every 10 minutes - can greatly improve your position fix:

Fix by 
depth soundings.

correct your soundings for tide, etc.;

copy the DR course line on a transparent sheet;

write the depths adjacent according to the times of the soundings;

move the sheet over the chart to find its best location.

Due to leeway, currents or other factors the two course lines need not be parallel to or of same length as each other.

Yacht charters and learning how to sail in Greece with instruction.
 

 

Overview

Line Of Position (LOP): The locus of points along which a ship's position must lie. A minimum of two LOP's are necessary to establish a fix. It is standard practice to use at least three LOP's when obtaining a fix, to guard against the possibility of and, in some cases, remove ambiguity.

Range or Distance LOP: Obtained by using a stadimeter, sextant or radar. A circle equal in radius to the measured distance is plotted about the navigation aid; the ship must be somewhere on this circle.

Running fix: A position determined by crossing lines of position obtained at different times and advanced or retired to a common time.

Dead reckoning: Determining a position by plotting courses and speeds from a known position. It is also used to predict when lights become visible or to determine the set and drift of a current. DR positions are drawn in advance to prevent sailing into danger. A DR position will be plotted:

  • every hour on the hour;
  • at the time of every course change or speed change;
  • for the time at which a (running) fix is obtained, also a new course line will be plotted;
  • for the time at which a single LOP is obtained;
  • and never draw a new course line from an EP position!

Estimated position: The most probable position of a craft determined from incomplete data or data of questionable accuracy. Such a position might be determined by applying a correction to the dead reckoning position, as for estimated current; by plotting a line of soundings; or by plotting a LOP of questionable accuracy.

Double angle on the bow: A method of obtaining a running fix by measuring the distance a vessel travels on a steady course while the relative bearing (right or left) of a fixed object doubles. The distance from the object at the time of the second bearing is equal to the run between bearings, neglecting drift.

Four point fix: A special case of doubling the angle on the bow, in which the first bearing is 45° right or left of the bow. Due to angular spread this is the most precise isosceles fix.

Special angle fix: A construction using special pairs of relative angles that give the distance travelled between bearings as equal to the navigation aids' range abeam.

Distance from horizon: The distance measured along the line of sight from a position above the surface of the earth to the visible horizon.

Sensible horizon: The circle of the celestial sphere formed by the intersection of the celestial sphere and a plane through the eye of the observer, and perpendicular to the zenith-nadir line.

Visible horizon: The line where Earth and sky appear to meet. If there were no terrestrial refraction, visible and geometrical horizons would coincide. Also called : apparent horizon.

Geometrical horizon: Originally, the celestial horizon; now more commonly the intersection of the celestial sphere and an infinite number of straight lines tangent to the earth's surface and radiating from the eye of the observer.

Dipping range or Geographic range: The maximum distance at which the curvature of the earth and terrestrial refraction permit an aid to navigation to be seen from a particular height of eye (without regard to the luminous intensity of the light).

Elevation: The height of the light above its chart datum in contrast to the height of the structure itself.

Chart Datum: Officially: Chart Sounding Datum: An arbitrary reference plane to which both heights of tides and water depths are expressed on a chart. In the same chart heights can be related to other datums than depths.

Vertical sextant angle: The method of using the subtended angle of a vertical object to find its range.

Index error: In a marine sextant the index error is primarily due to lack of parallelism of the index mirror and the horizon glass at zero reading. A positive index error is subtracted and a negative index error is added.

Estimation with horizon: Estimation of heights using the horizon: All tops crossing the horizon and with bases at sea level are on eye level.

Estimation with depth effect: .

Estimated position with soundings:

موقعیت یابی برای ناوبری ساحلی (Positions)

منبع : حمل و نقل دریایی

موقعیت یابی برای ناوبری ساحلی (Positions)

Positions

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Longitude and latitude

The earth can be regarded as a spherical object, and since we're dealing with a 3-dimensional shape we need coordinates of a different form than the usual x- and y-axes. Though adding an extra z-axes would make sense for submarines, we will most likely be found on the surface of this sphere while using another system of coordinates, parallels of latitude
 and meridians of longitude.that covers our planet with imaginary lines called meridians and parallels, see figure 1. All these lines together provide the grid which enables us to describe any position in longitudes and latitudes.

The obvious place to divide the Northern and Southern Hemispheres was the equator. But the division of the Eastern and Western hemispheres was the source of much political turmoil. Greenwich (Great Britain) won, placing for example The Netherlands in the Eastern and Ireland in the Western Hemisphere.

It takes the earth 24 hours for a full rotation of 360°. Thus, every hour we rotate 15° longitude, see figure 2.

When it is 12:00 UTC (international standard time) - anywhere in the world - it is 12:00 Local Time in Greenwich and 24:00 Local Time at the other side of the planet: 180° E or 180° W: the date line. Crossing this special meridian changes not only the hour but also the date.

prime meridian international date line and time zones The North Pole has a latitude of 90° N and the South Pole 90° S. The meridians cover twice this angle up to 180° W or E.
Meridians converge at the poles, whereas parallels run parallel to each other and never meet. All meridians and the equator - the biggest parallel - form great circles, and the remaining parallels form so-called small circles. A great circle divides the earth in two exact halves.

In figure 3 the position of Boston in the United States is shown using latitude and longitude in degrees, minutes and seconds:
42° 21' 30" N , 71° 03' 37" W

Most sailors will actually notate seconds in metric fractions of minutes:
42° 21,5' N , 71° 03,6' W or
42° 21.5' N , 71° 03.6' W, see the notation style guide

On small scaled charts we want to be accurate within one minute or one nautical mile. On larger scaled charts the accuracy is more likely to be within a tenth of a mile (a cable).

If the earth were a perfect sphere with a circumference of roughly 40000 kilometres all great circles - meridians plus the equator - would have the same length and could be used as a distance unit when divided longitude and latitudeinto 360 degrees, or 360° x 60' = 21600' minutes. In 1929, the international community agreed on the definition of 1 international nautical mile as 1852 metres, which is roughly the average length of one minute of latitude i.e. one minute of arc along a line of longitude (a meridian).
Or to put it shortly: 1 nm = 1'

We are now able to describe any position in latitudes and longitudes. Moreover, we can state the distance between two of those positions using nautical miles or minutes. All we need now is a proper way to define speed. For that, sailors use knots, the number of nautical miles an hour.

RYA & ASA sailing schools

To put this navigation course into practice a Royal Yachting Association or American Sailing Association approved sailing course is recommended. Sailing schools in Greece and Turkey for:
RYA competent crew
RYA day skipper (non-tidal)
RYA coastal skipper (non-tidal)
ASA basic coastal cruising (103)
ASA bareboat chartering (104)
ASA coastal navigation (105)
And the most enjoyable way to learn how to sail is by combining such courses with a yachting vacation in Greece or Turkey. Ideal areas for sailing courses are the Saronic Gulf near Athens and the Ionian Islands to the west of Greece, which provide reliable and gentle winds, dolphins and ancient Greek monuments and temples.

A little History

Mariners during the 15th century relied on charts called "portolans" to assist them on their voyages. Portolan comes from the Italian word portolani, which were medieval pilot books.

The portolans contained maps of coastlines, locations of harbours, river mouths, and man-made features visible from the sea. A 15th century 
portolano. They were a compilation of centuries of seafarer observations. As sailors' skills improved and the use of the compass was more widespread, portolans improved in accuracy.

Also Columbus used these portolans on his journeys. Portuguese chart makers added the meridian line, a point useful for latitude sailing as well as for navigating solely by compass. A geographic feature could now be located through the use of its distance in degrees of latitude from a ship's point of departure. Note that the use of latitude and longitude was understood since the time of Ptolemy, the second century CE.

During the fifteenth century Portugal led the European world in sea exploration. The golden age of discovery for Portugal lasted almost a century until the Dutch eventually seized their trade routes from them.
As we move to the next chapter of this course we enter the sixteenth century when the Mercator chart was invented.

Glossary

Parallels: Circles parallel to the equator, ranging from 0° to 90° N or S. Only the equator is a great circle.

Meridians: half-circles converging at the poles, ranging from 0° to 180° E or W. Each pair of opposing meridians forms a great circle.

Prime meridian: 0° or the Greenwich meridian which - together with the date line meridian - divides the Western and Eastern hemispheres.

Great circle: The intersection of a sphere and a plane that passes through the sphere's centre.

Small circle: The intersection of a sphere and a plane that doesn't pass though the sphere's centre.

Time zones: By convention 24 zones, each 15° longitude wide. Hence, noon at Greenwich gives midnight at 180° E.

GMT, UTC, Zulu: The outdated accronym GMT (Greenwich Mean Time) is roughly the same as UTC or Zulu, and is also the local time at Greenwich when daylight saving isn't used. Note that UTC is an atomic time scale which only approximates GMT, so best to use the modern term “UTC”. Antonym: Local time elsewhere. For example, local time in Athens = UTC + 2.

Date line: The 180° meridian which extends from or is opposite to the prime meridian. Here, not only the hour changes when crossing the meridian, but also the date.

Latitude: Position property defined by the number of degrees north or south of the equator, varies from 0° to 90°.

Longitude: Position property defined by the number of degrees east or west of the prime meridian, varies from 0° to 180°.

Position: Latitude first and longitude second. For example: Athens in Greece 37° 58' N , 23° 43' E.

Nautical mile: One nm is one minute (') on the vertical scale on the chart. 1' equals 1852 metres. Nautical miles are divided into 10 cables.

Knots: Nautical miles per hour.

قطب نماهای ناوبری (Compass navigation) و نیاز آن برای نقشه های دریایی

منبع : حمل و نقل دریایی

قطب نماهای ناوبری (Compass navigation) و نیاز آن برای نقشه های دریایی

Compass navigation

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Marine compass

In China compasses have been in use since the Han dynasty (2nd century BCE to 2nd century CE) when they were referred to as “south-pointers”. However at first these magnets were only used for geomancy much like in the art of Feng Shui.

Eventually, during the Sung dynasty (1000 CE) many trading ships were then able to sail as far as Saudi Arabia using compasses for marine navigation. Between 1405 and 1433, Emperor Chu Ti's Treasure Fleet of the Dragon Throne ruled the entire South Pacific and the Indian Ocean, a territory that ranges from Korea and Japan to the Eastern coast of Africa.

At this time Western mariners were still rather ignorant of the navigational use of the magnet. Petrus Perigrinus van Maricourt wrote a first treatise on the magnet itself: “De Magnete” (1269). And though its nautical use was already mentioned in 1187 by the English monk Alexander Neckham, the use onboard only came about around the 13th and 14th century in the Mediterranean Sea.

Much later, in 1545, Pedro de Medina (Sevilla 1493-1567) wrote the Spanish standard work “Arte de Navegar” on marine compass navigation. This masterpiece was first translated in Dutch (1580) and was -O Irony- used by Jacob van Heemskerk when the Dutch destroyed the Spanish fleet near Gibraltar in 1607. The drawback was of course Van Heemskerk's own death during this victory.

Magnetic Variation

In the fin-de-siècle of the sixteenth century mariners believed that the magnetic north pole coincided with the geographic north pole. Any suggestion otherwise had been denied by Pedro de Medina. قطب نماهای ناوبری (Compass navigation) و نیاز آن برای نقشه های دریایی

Magnetic observations made by explorers in subsequent decades showed however that these suggestions were true. But it took until the early nineteenth century, to pinpoint the magnetic north pole somewhere in Arctic Canada (78° N , 104° W). From then on the angle between the true North and the Magnetic North could be precisely corrected for. This correction angle is called magnetic variation or declination.

It is believed that the Earth's magnetic field is produced by electrical currents that originate in the hot, liquid, outer core of the rotating Earth. The flow of electric currents in this core is continually changing, so the magnetic field produced by those currents also changes. This means that at the surface of the Earth, both the strength and direction of the magnetic field will vary over the years. This gradual change is called the secular variation of the magnetic field. Therefore, variation changes not only with the location of a vessel on the earth but also varies in time.

The correction for magnetic variation for your location is shown on the nearest! nautical chart's compass rose. In this example we find a variation of 4° 15' W in 2009, with an indicated annual correction of 0° 08' E. Hence, in 2011 this variation is estimated to be 3° 59', almost 4° West. This means that if we sail 90° on the chart (the true course), the compass would read 94°.

Another example: let's say the compass rose gives a variation of 2° 50' E in 2007, with a correction of 0° 04' E per year. In 2009 this variation is estimated to be 2° 58', almost 3° East. Now, if we sail 90° on the chart, the compass would read 87°.

Correcting for variation

Difference between true course and magnetic course These overlayed compass roses show the difference between true north and magnetic north when the magnetic variation is 10° West.

From the image we find: tc = cc + var
in which “cc” and “tc” stand for “compass course” and “true course”, respectively.

To convert a true course into a compass course we need first assign a “-” to a Western and a “+” to a Eastern variation. Note that this makes sense! because of the clockwise direction of the compass rose. Here, the inner circle is turned 10° anticlockwise, hence -10°.
Now, use the same but re-written equation:
cc = tc - var
235° = 225° - (-10°)
So, to sail a true course of 225°, the helmsman has to steer a compass course of 235°.

To convert a compass course into a true course we can use the original equation. If we have steered a compass course of 200°, we have to plot a true course of 203° in the chart if the variation is 3° East or a true course of 190° if the variation is 10° West.

Magnetic deviation

Magnetic deviation is the second correctable error. The deviation error is caused by magnetic forces within your particular boat. Pieces of metal, such as an engine or an anchor, can cause magnetic forces. And also stereo and other electric equipment or wiring, if too close to the compass, introduce errors in compass heading.

Furthermore, the deviation changes with the ship's heading, resulting in a deviation table as shown below. The vertical axis states the correction in degrees West or East, where East is again positive.

Deviation 
table: 

For each heading 

a different deviation correction 

is needed.


The horizontal axis states the ship's heading in degrees divided by ten. Thus, when you sail a compass course of 220°, the deviation is 4° W. (Note, that on most modern sailing yachts the deviation is usually not larger than 3°).

When a compass is newly installed it often shows larger deviations than this and needs compensation by carefully placing small magnets around the compass. It is the remaining error that is shown in your deviation table.
You can check your table every now and then by placing your boat in the line of a pair of leading lights and turning her 360 degrees.

Correcting for both deviation and variation

Converting a compass course into a true course, we can still use our equation but we need to add the correction for deviation:
cc + var + dev = tc

Example 1: The compass course is 330°, the deviation is +3° (table) and the variation is +3° (chart);
330° cc + 3° var + 3° dev = ?° tc
giving a true course of 336° which we can plot in our chart

Example 2: The compass course is 220°, the deviation is -4° (table) and the variation is still +3° (chart).
220° cc + 3° var + -4° dev = ?° tc
giving a true course of 219°.

Example 3: The compass course is still 220°, therefore the deviation is still -4° (table) but let's use a variation of -10° this time.
220° cc + -10° var + -4° dev = ?° tc
giving a true course of 206°.

Converting a true course into a compass course is a little less straight forward, but it is still done with the same equation.

Example 4: The true course from the chart is 305° and the variation is +3° (chart), yet we don't know the deviation;
?° cc + 3° var + ?° dev = 305° tc
Luckily, we can rewrite this so this reads:
cc + dev = 305° tc - + 3° var = 302°
In plain English: the difference between the true course and the variation (305 - + 3) = 302 should also be the summation of the compass course and the deviation. So, we can tell our helms person to steer 300°, since with a cc of 300° we have a deviation of +2° (As can be deduced from the deviation table above).

Example 5: The true course from the chart is 150° and we have a Western variation of 7 degrees (-7°). We will use the rewritten equation to get:
150° tc - - 7° var = cc + dev = 157°
From the deviation table we find a compass course of 160° with a deviation of -3°.
Voilà!

Magnetic course

The magnetic course (mc) is the heading after magnetic variation has been considered, but without compensation for magnetic deviation. This means that we are dealing with the rewritten equation from above:
tc - var = cc + dev = mc.

Magnetic courses are used for three reasons:Three types of North - compass, magnetic, true

To convert a true course into a compass course like we saw in the last paragraph.

On vessels with more than one steering compass, also more deviation tables are in use; hence only a magnetic or true course is plotted in the chart.

Bearings taken with a handheld compass often don't require a correction for deviation, and are therefore useful to plot in the chart as magnetic courses.


Note, that the actual course lines the navigator draws in the chart are always true courses! These can subsequently be labeled with the true course or the corresponding magnetic or compass course if appropriate. In the next chapter we will be plotting courses in the chart.

To summarise, we have three types of “north” (true, magnetic and compass north) like we have three types of courses: tc, mc and cc. All these are related by deviation and variation.

Glossary

Maps with isogonic lines:
World - overview 2000
World - detailed 2000
World - detailed 2005
World - animated in time
Variation: The angle between the magnetic north pole and the geographic north pole. Also called the magnetic declination.

Secular variation: The change of magnetic declination in time with respect to both strength and direction of its magnetic field.

West (-) , East (+): Western variations or deviations are designated with a negative sign by convention due to the compass card's clockwise direction.

Deviation: The error in compass heading caused by electric magnetic currents and or metal objects.

Deviation table: A table containing deviations in degrees versus the ship's heading (compass course) in degrees. Usually plotted in a graph.

True course: Course plotted in the chart i.e. course over the ground or “course made good”. The course corrected for compass errors.

Compass course: The course (ship's heading) without the correction for compass errors.

cc + var + dev = tc: This equation shows the connection between the compass course, its errors and the true course. It can also be read as: tc - var = cc + dev


وب سایت ناوبری دریایی و دریانوردی در یونان و ترکیه

وب سایت ناوبری دریایی و دریانوردی در یونان و ترکیه

www.sailingissues.com

http://www.sailingissues.com

وب سایت آزاد و شخصی ارائه اطلاعات منحصر به فرد در ناوبری دریایی و دریانوردی در یونان و ترکیه ...

You have reached SailingIssues.com, a free and personal website providing unique information on marine navigation and sailing holidays in Greece and Turkey. This website continuously grows and has already become one of the leading Internet resources on Greek and Turkish yacht charter holidays, ahead of the typical commercial travel sites.

Free advice on yacht charter companies
Many visitors have shared their charter experiences with me. Moreover, I myself have made the mistake of sailing with inferior companies before finding the more trustworthy charter companies. So, if you would like independent advice on reliable yacht charters or sailing schools, you are welcome.

Yacht charters and sailing holidays in the Saronic Charter yachts and sailing holidays in the Ionian Sea Charter holidays in the Dodecanese
Argolic - Saronic
Athens
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Charter yachts and sailing holidays in the Northern Sporades Yacht charters and sailing holidays in the Cyclades Yacht charter holidays in Turkey
Northern Sporades
 
Cyclades
 
Turkey: Lycian,
Carian, Ionian


منبع : حمل و نقل دریایی

دانلود کتاب مقدمه ای بر ناوبری نجومی (ashort guide to celestial navigation)

کتابی مناسب برای مشاهدات و محاسبات نجومی

A Short Guide to Celestial Navigation

Copyright © 1997-2011 Henning Umland
Permission is granted to copy, distribute and/or modify this document under the terms of the
GNU Free Documentation License, Version 1.3 or any later version published by the Free
Software Foundation; with no Invariant Sections, no Front-Cover Texts and no Back-Cover
Texts. A copy of the license is included in the section entitled "GNU Free Documentation
License".

Revised October 1st, 2011
First Published May 20th, 1997

در فرمت فشرده (zip)

برای دانلود کلیک کنید...

http://www.celnav.de/astro.zip

مجموعه مقالات معتبر لاتین مهندسی ساحل و دریا از سال 2002 تا 2012 (Coastal Engineering)

منبع : سیویلیا

مجموعه مقالات معتبر لاتین مهندسی ساحل و دریا از سال 2002 تا 2012 (Coastal Engineering)

This international journal is indispensable reading for engineers working in the field of marine and coastal technology. Combining practical application with modern technological and scientific achievements, it publishes fundamental studies as well as case histories on the following aspects of coastal, harbour and offshore engineering: studies on waves and currents; coastal morphology; estuary hydraulics; harbour and offshore structures. Mathematical and physical models as well as constructional aspects and environmental problems relating to these items are also included. Each publication should have as a minimum one paragraph stressing practical engineering applications.


Volume 44, Issue 3, Pages EX1-EX2, 191-274 (January 2002)

Size: 1.7 MB | Format: PDF

1.Morphological changes of the Haringvliet estuary after closure in 1970
Pages 191-203
I.E Tönis, J.M.T Stam, J van de Graaf
2.Simplified higher-order Boussinesq equations: I. Linear simplifications
Pages 205-229
Andrew B. Kennedy, James T. Kirby, Mauricio F. Gobbi
3.Limiting criteria of permanent progressive waves
Pages 231-237
Samir Abohadima, Masahiko Isobe
4.Linear waves propagating over a rapidly varying finite porous bed
Pages 239-260
Rodolfo Silva, Paulo Salles, Arturo Palacio
5.Polynomial approximations for Fresnel integrals in diffraction analysis
Pages 261-266
Michael E McCormick, David R.B Kraemer

6.Comments on “Forced and self-organized shoreline response for a beach in the southern Baltic Sea determined through singular spectrum analysis” [Coast. Eng. 43 (2001) 41–58]

Pages 267-269
D.E Reeve

7.Reply to the comments on “Forced and self-organized shoreline response for a beach in the southern Baltic Sea determined through singular spectrum analysis” [Coast. Eng. 43 (2001) 41–58]

Pages 271-272
G Róz°ynski
8.Reply to reply to comments on “Forced and self-organized shoreline response for a beach in the southern Baltic Sea determined through singular spectrum analysis” [Coast. Eng. 43 (2001) 41–58]
Pages 273-274
D.E. Reeve

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Volume 44, Issue 4, Pages 275-352 (February 2002)

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1.An investigation of the velocity field under regular and irregular waves over a sand beach
Pages 275-300
J.C Doering, A.J Baryla
2.Transport of waste heat from a nuclear power plant into coastal water
Pages 301-319
Ping Zeng, Huiquan Chen, Baichuan Ao, Ping Ji, Xiaojian Wang, Zhiliang Ou
3.Application of wavelet transform analysis to landslide generated waves
Pages 321-338
Andrea Panizzo, Giorgio Bellotti, Paolo De Girolamo
4.Stem waves along vertical wall due to random wave incidence
Pages 339-350
Hajime Mase, Tetsu Memita, Masatoshi Yuhi, Toshikazu Kitano
5.Contents of volume 44
Pages 351-352

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Volume 45, Issue 1, Pages 1-70 (March 2002)

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1.Modelling intensive near-bed sand transport under wave–current flow versus laboratory and field data
Pages 1-18
Leszek M Kaczmarek, Rafal Ostrowski
2.Nearshore bar crest location quantified from time-averaged X-band radar images
Pages 19-32
B.G Ruessink, P.S Bell, I.M.J van Enckevort, S.G.J Aarninkhof
3.Wave runup, transmission, and reflection for structures armored with CORE-LOC®
Pages 33-52
Ivano Melito, Jeffrey A Melby
4.Shear stress and sediment transport calculations for swash zone modelling
Pages 53-60
Peter Nielsen
5.Vertical fluxes of sediment in oscillatory sheet flow
Pages 61-68
Peter Nielsen, Koen van der Wal, Luke Gillan
6.Erratum to “Scour around coastal structures: a summary of recent research” [Coastal Eng. 44 (2001) 153–190]
Page 69
B Mutlu Sumer, Richard J.S Whitehouse, Alf Tørum

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Volume 45, Issue 2, Pages 71-126 (April 2002)

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 1.Simple and explicit solution of wave dispersion equation
Pages 71-74
Junke Guo
2.Intense near-bed sediment motions in waves and currents
Pages 75-87
Ping Dong, Kefeng Zhang
3.An integral swash zone model with friction: an experimental and numerical investigation
Pages 89-110
R. Archetti, M. Brocchini
4.Influence of infiltration on suspended sediment under waves
Pages 111-123
C. Obhrai, P. Nielsen, C.E. Vincent
5.Shore Management Guidelines: written by K. Mangor, Published by DHI Water and Environment, Denmark (232 pp.). Price: DKK 250, ISBN 87-981950-9-3.
Page 125
J.W. Kamphuis

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Volume 45, Issues 3-4, Pages 127-286 (May 2002)

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 Surface and Swash Zone Mechanics

1.Surf and Swash Zone Mechanics Contents
Page iv
2.Introduction to the special issue “Surf- and swash-zone processes”
Page 127
Jorgen Fredsoe
3.Turbulence in the swash and surf zones: a review
Pages 129-147
Sandro Longo, Marco Petti, Inigo J. Losada
4.Hydrodynamics and sediment transport in the swash zone: a review and perspectives
Pages 149-167
Berry Elfrink, Tom Baldock
5.Vertical variation of the flow across the surf zone
Pages 169-198
Erik Damgaard Christensen, Dirk-Jan Walstra, Narumon Emerat
6.Morphodynamic modelling of rip channel growth
Pages 199-221
Jesper Damgaard, Nick Dodd, Lisa Hall, Tim Chesher
7.An experimental study of rip channel flow
Pages 223-238
Nils Drønen, Harshinie Karunarathna, Jørgen Fredsøe, B. Mutlu Sumer, Rolf Deigaard
8.Reduction of sand demand for shore protection
Pages 239-259
Arved J. Raudkivi, Hans-H. Dette
9.Modelling morphological processes in the vicinity of shore-parallel breakwaters
Pages 261-284
Julio A. Zyserman, Hakeem K. Johnson
10.Contents of volume 45
Pages 285-286
 
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Volume 46, Issue 1, Pages 1-88 (June 2002)

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1.Intercomparison of research and practical sand transport models
Pages 1-23
A.G Davies, L.C van Rijn, J.S Damgaard, J van de Graaff, J.S Ribberink
2.A numerical model for wave motions and turbulence flows in front of a composite breakwater
Pages 25-50
Tian-Jian Hsu, Tsutomu Sakakiyama, Philip L.-F. Liu
3.Statistical distribution of wave-surface elevation for second-order random directional ocean waves in finite water depth
Pages 51-60
Jin-Bao Song, Yi-Jun Hou, Yi-Jun He, Yong-Hong Wu, Bao-Shu Yin
4.Phase lags in oscillatory sheet flow: experiments and bed load modelling
Pages 61-87
C.Marjolein Dohmen-Janssen, David F. Kroekenstoel, Wael N. Hassan, Jan S. Ribberink

 
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Volume 46, Issue 2, Pages 89-158 (July 2002)

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1.Modeling wave runup with depth-integrated equations
Pages 89-107
Patrick J. Lynett, Tso-Ren Wu, Philip L.-F. Liu
2.Controlling spatial oscillations in bed level update schemes
Pages 109-126
Hakeem K. Johnson, Julio A. Zyserman
3.Changes in coastal sediment transport processes due to construction of New Damietta Harbour, Nile Delta, Egypt
Pages 127-138
Hesham M El-Asmar, Kevin White
4.Unsteady air bubble entrainment and detrainment at a plunging breaker: dominant time scales and similarity of water level variations
Pages 139-157
Hubert Chanson, Shin-ichi Aoki, Mamoru Maruyama
 
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Volume 46, Issue 3, Pages 159-248 (August 2002)

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1.Editorial Board
Page IFC
2.Stochastic simulation of episodic soft coastal cliff recession
Pages 159-174
Jim W Hall, Ian C Meadowcroft, E.Mark Lee, Pieter H.A.J.M van Gelder
3.Temporal and spatial variations of surf-zone currents and suspended sediment concentration
Pages 175-211
Ping Wang, Bruce A Ebersole, Ernest R Smith, Bradley D Johnson
4.Analytical solutions for storm tide codes
Pages 213-231
Rodney J. Sobey
5.Field experiment on secondary wave generation on a barred beach and the consequent evolution of energy dissipation on the beach face
Pages 233-247
N Sénéchal, P Bonneton, H Dupuis
 
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Volume 46, Issue 4, Pages EX1-EX2, 249-316 (September 2002)

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1.Editorial Board
Page IFC
2.Modelling of wave loads and hydraulic performance of vertical permeable structures
Pages 249-276
S. Requejo, C. Vidal, I.J. Losada
3.Regeneration of sand waves after dredging
Pages 277-289
M.A.F Knaapen, S.J.M.H Hulscher
4.Laboratory study of wave and turbulence characteristics in narrow-band irregular breaking waves
Pages 291-313
Francis C.K Ting
5.Contents of volume 46
Page 315

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Volume 47, Issue 1, Pages EX1-EX2, 1-78 (November 2002)

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1.A 2D numerical model of wave run-up and overtopping
Pages 1-26
Matthew E. Hubbard, Nick Dodd
2.Wave scattering by a submerged plate in presence of a steady uniform current
Pages 27-34
Vincent Rey, Régis Capobianco, Cyril Dulou
3.Geometry, migration and evolution of small-scale bedforms generated by regular and irregular waves
Pages 35-52
C Faraci, E Foti
4.Bars formed by horizontal diffusion of suspended sediment
Pages 53-75
Kerry P Black, Richard M Gorman, Karin R Bryan
5.Erratum to “Controlling spatial oscillations in bed level update schemes” [Coastal Engineering 46 (2002) 109–126]
Page 77
Hakeem K Johnson, Julio A Zyserman
 
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Volume 47, Issue 2, Pages EX1-EX2, 79-264 (December 2002)

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 Shore Nourishment in Europe

1.Contents
Page iv
2.Preface
Pages 79-80
Christos Fragakis
3.Beach nourishment projects, practices, and objectives—a European overview
Pages 81-111
H Hanson, A Brampton, M Capobianco, H.H Dette, L Hamm, C Laustrup, A Lechuga, R Spanhoff
4.Nourishment design and evaluation: applicability of model concepts
Pages 113-135
Michele Capobianco, H Hanson, M Larson, H Steetzel, M.J.F Stive, Y Chatelus, S Aarninkhof, T Karambas
5.Application of prototype flume tests for beach nourishment assessment
Pages 137-177
H.H Dette, M Larson, J Murphy, J Newe, K Peters, A Reniers, H Steetzel
6.Gradation effects in sediment transport
Pages 179-210
R.J de Meijer, J Bosboom, B Cloin, I Katopodi, N Kitou, R.L Koomans, F Manso
7.Variability of shore and shoreline evolution
Pages 211-235
Marcel J.F Stive, Stefan G.J Aarninkhof, Luc Hamm, Hans Hanson, Magnus Larson, Kathelijne M Wijnberg, Robert J Nicholls, Michele Capobianco
8.A summary of European experience with shore nourishment
Pages 237-264
L Hamm, M Capobianco, H.H Dette, A Lechuga, R Spanhoff, M.J.F Stive
 
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Volume 47, Issue 3, Pages 265-366 (January 2003)

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1.An approach to determining nearshore bathymetry using remotely sensed ocean surface dynamics
Pages 265-293
Shubhra K Misra, Andrew B Kennedy, James T Kirby
2.The predictability of cross-shore bed evolution of sandy beaches at the time scale of storms and seasons using process-based Profile models
Pages 295-327
L.C van Rijn, D.J.R Walstra, B Grasmeijer, J Sutherland, S Pan, J.P Sierra
3.Numerical estimation of the wave forces acting on a three-dimensional body on submerged breakwater
Pages 329-345
Dong-Soo Hur, Norimi Mizutani
4.Shear stress and sediment transport calculations for sheet flow under waves
Pages 347-354
Peter Nielsen, David P. Callaghan
5.Settlement of vertical piles exposed to waves
Pages 355-365
J Carreiras, J.Antunes do Carmo, F Seabra-Santos
 
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Volume 47, Issue 4, Pages 367-444 (February 2003)

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1.Experiments on the reflection coefficients of a detached breakwater in a directional wave field
Pages 367-379
Wei-Po Huang, Chun-Ren Chou, John Z Yim
2.A synchronously coupled tide–wave–surge model of the Yellow Sea
Pages 381-398
Byung Ho Choi, Hyun Min Eum, Seung Buhm Woo
3.Bailard's sediment transport formulation in shelf sea conditions: comparison with observations using a clustering technique
Pages 399-412
Johan van der Molen
4.Modeling erosion of sedimentary coasts in the western Russian Arctic
Pages 413-429
I.O. Leont'yev
5.The wave plus current flow over vortex ripples at an arbitrary angle
Pages 431-441
Ken Haste Andersen, Carla Faraci
6.Contents of volume 47
Pages 443-444

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Volume 48, Issue 1, Pages EX1-EX2, 1-74 (March 2003)

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1.Validation and intercomparisons of wave measurements and models during the EuroROSE experiments
Pages 1-28
L.R Wyatt, J.J Green, K.-W Gurgel, J.C Nieto Borge, K Reichert, K Hessner, H Günther, W Rosenthal, O Saetra, M Reistad
2.Probability assessment for deep-draft navigation channel design
Pages 29-50
Michael J. Briggs, Leon E. Borgman, Eivind Bratteland
3.Limiting slopes and depths at ebb-tidal shoals
Pages 51-65
Frank S Buonaiuto, Nicholas C Kraus
4.On the discrepancy in long wave scaling
Pages 67-74
Chandrasekher Narayanan
 
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Volume 48, Issue 2, Pages EX1-EX2, 75-138 (April 2003)

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1.Wave forces on submerged, alternately submerged, and emerged semicircular breakwaters
Pages 75-93
Dekui Yuan, Jianhua Tao
2.Longshore sediment transport rate—measurement and estimation, central west coast of India
Pages 95-109
V Sanil Kumar, N.M Anand, P Chandramohan, G.N Naik
3.Comparison of sediment transport formulae for the coastal environment
Pages 111-132
Benoi^t Camenen, Philippe Larroudé
4.Discussion of “Simple and explicit evolution to the wave dispersion equation” [Coastal Engineering 45 (2002) 71–74]
Pages 133-135
Zai-Jin You
5.Reply to ‘Discussion of “Simple and explicit solution to the wave dispersion equation” [Coastal Engineering 45 (2002) 71–74]’
Page 137
Junke Guo
 
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Volume 48, Issue 3, Pages EX1-EX2, 139-210 (June 2003)

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1.Calibration and verification of a parametric wave model on barred beaches
Pages 139-149
B.G Ruessink, D.J.R Walstra, H.N Southgate
2.Data-driven modeling of multiple longshore bars and their interactions
Pages 151-170
Grzegorz Rózynski
3.A simple model of unsteady sheet-flow sediment transport
Pages 171-188
J Malarkey, A.G Davies, Z Li
5.The drag coefficient, bottom roughness, and wave-breaking in the nearshore
Pages 189-195
Falk Feddersen, E.L Gallagher, R.T Guza, Steve Elgar
6.Mathematical modelling of sand wave migration and the interaction with pipelines
Pages 197-209
Robin Morelissen, Suzanne J.M.H Hulscher, Michiel A.F Knaapen, Attila A Németh, Romke Bijker
 
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Volume 48, Issue 4, Pages EX1-EX2, 211-290 (July 2003)

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1.Evaluation of a method to reduce uncertainty in wind hindcasts performed with regional atmosphere models
Pages 211-225
R. Weisse, F. Feser
2.Scour below pipelines and around vertical piles in random waves
Pages 227-242
Dag Myrhaug, Håvard Rue
3.Effects of cross-shore boundary condition errors in nearshore circulation modeling
Pages 243-256
Qin Chen, Ib A. Svendsen
4.An unsteady wave driver for narrowbanded waves: modeling nearshore circulation driven by wave groups
Pages 257-275
Andrew B. Kennedy, James T. Kirby
5.Extended mild-slope equation for random waves
Pages 277-287
Changhoon Lee, Gunwoo Kim, Kyung-Duck Suh
6.Contents of volume 48
Pages 289-290

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Volume 49, Issues 1-2, Pages EX1-EX2, 1-154 (August 2003)

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1.Structural permeability effects on the interaction of a solitary wave and a submerged breakwater
Pages 1-24
Ching-Jer Huang, Hsing-Han Chang, Hwung-Hweng Hwung
2.Fixed absorbing semi-immersed breakwater
Pages 25-41
J. Brossard, A. Jarno-Druaux, F. Marin, E.H. Tabet-Aoul
3.Suspended sediment transport under seiches in circular and elliptical basins
Pages 43-70
David Pritchard, Andrew J. Hogg
4.Internal generation of waves in 2D fully elliptic mild-slope equation FEM models
Pages 71-81
Giorgio Bellotti, Gian Mario Beltrami, Paolo De Girolamo
5.Characteristics of pressure pulses propagating through water-filled cracks
Pages 83-98
G. Müller, G. Wolters, M.J. Cooker
6.A curvilinear version of a quasi-3D nearshore circulation model
Pages 99-124
Fengyan Shi, Ib A. Svendsen, James T. Kirby, Jane McKee Smith
7.Wave field modification by bathymetric anomalies and resulting shoreline changes: a review with recent results
Pages 125-153
Christopher J. Bender, Robert G. Dean

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Volume 49, Issue 3, Pages EX1-EX2, 155-238 (September 2003)

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1.Effect of externally generated turbulence on wave boundary layer
Pages 155-183
Jørgen Fredsøe, B.Mutlu Sumer, Andrzej Kozakiewicz, Lloyd H.C Chua, Rolf Deigaard
2.Modeling of waves and currents in the nearshore parametric vs. probabilistic approach
Pages 185-207
B.T. Grasmeijer, B.G. Ruessink
3.On berm breakwaters. Stability, scour, overtopping
Pages 209-238
Alf Tørum, Franziska Kuhnen, Andreas Menze

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Volume 49, Issue 4, Pages 239-308 (October 2003)

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1.Moving shoreline boundary condition for nearshore models
Pages 239-261
R.S. Prasad, I.A. Svendsen
2.Reversed responses within a segmented detached breakwater, the Tuscany coast Italy—a case study
Pages 263-274
Dan Bowman, Enzo Pranzini
3.A video-based technique for mapping intertidal beach bathymetry
Pages 275-289
Stefan G.J Aarninkhof, Ian L Turner, Thomas D.T Dronkers, Mark Caljouw, Leann Nipius
4.Phase-decoupled refraction–diffraction for spectral wave models
Pages 291-305
L.H. Holthuijsen, A. Herman, N. Booij
5.Contents of volume 49
Page 307

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Volume 50, Issues 1-2, Pages 1-84 (November 2003)

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1.Experimental study of marine pipelines on unstable and liquefied seabed
Pages 1-17
T.C Teh, A.C Palmer, J.S Damgaard
2.Modelling waves and currents at the LSTF and other laboratory facilities
Pages 19-45
Ib A Svendsen, Wenkai Qin, Bruce A Ebersole
3.The reflection of oblique incident waves by breakwaters with double-layered perforated wall
Pages 47-60
Yucheng Li, Guohai Dong, Hongjie Liu, Dapeng Sun
4.Wave transformation by two-dimensional bathymetric anomalies with sloped transitions
Pages 61-84
Christopher J Bender, Robert G Dean

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Volume 50, Issue 3, Pages 85-166 (January 2004)

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Volume 50, Issue 4, Pages 167-242 (February 2004)

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Volume 51, Issue 1, Pages 1-102 (March 2004)

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Volume 51, Issue 2, Pages 103-206 (April 2004)

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Volume 51, Issue 3, Pages 207-276 (May 2004)

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Volume 51, Issue 4, Pages 277-336 (June 2004)

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Volume 51, Issues 5–6, Pages 337-530 (August 2004)

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Volume 51, Issue 7, Pages 531-656 (September 2004)

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Volume 51, Issues 8–9, Pages 657-940 (October 2004)

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Volume 51, Issue 10, Pages 941-1066 (November 2004)

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Volume 51, Issues 11–12, Pages 1067-1188 (December 2004)

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Volume 52, Issue 1, Pages 1-102 (January 2005)

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Volume 52, Issue 2, Pages 103-202 (February 2005)

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Volume 52, Issue 3, Pages 203-312 (March 2005)

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Volume 52, Issue 4, Pages 313-390 (April 2005)

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Volume 52, Issue 5, Pages 391-472 (May 2005)

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Volume 52, Issue 6, Pages 473-564 (June 2005)

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Volume 52, Issue 7, Pages 565-654 (July 2005)

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Volume 52, Issue 8, Pages 655-726 (August 2005)

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Volume 52, Issue 9, Pages 727-814 (September 2005)

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Volume 52, Issues 10–11, Pages 815-1126 (November 2005)

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Volume 52, Issue 12, Pages 1127-1192 (December 2005)

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Volume 53, Issue 1, Pages 1-118 (January 2006)

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Volume 53, Issues 2–3, Pages 119-310 (February 2006)

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Volume 53, Issue 4, Pages 311-394 (March 2006)

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Volume 53, Issues 5–6, Pages 395-544 (April 2006)

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Volume 53, Issue 7, Pages 545-630 (May 2006)

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Volume 53, Issue 8, Pages 631-710 (June 2006)

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http://www.4shared.com/rar/JGG4fm9V/Volume_53_Issue_8_Pages_631-71.html

Volume 53, Issue 9, Pages 711-798 (July 2006)

Size: 3.9 MB | Format: PDF | Quality: Original preprint
 
http://www.4shared.com/rar/V6bMLK43/Volume_53_Issue_9_Pages_711-79.html

Volume 53, Issue 10, Pages 799-878 (September 2006)

Size: 6.7 MB | Format: PDF | Quality: Original preprint
 
http://www.4shared.com/rar/PWmMMNiO/Volume_53_Issue_10_Pages_799-8.html

Volume 53, Issue 11, Pages 879-982 (November 2006)

Size: 11.2 MB | Format: PDF | Quality: Original preprint
 
http://www.4shared.com/rar/-9qFi5Ma/Volume_53_Issue_11_Pages_879-9.html

Volume 53, Issue 12, Pages 983-1062 (December 2006)

Size: 6.3 MB | Format: PDF | Quality: Original preprint
 
http://www.4shared.com/rar/iFoM0OO7/Volume_53_Issue_12_Pages_983-1.html

Volume 54, Issue 1, Pages 1-90 (January 2007)

Size: 11.7 MB | Format: PDF | Quality: Original preprint
 
http://www.4shared.com/rar/oBiyKdKN/Volume_54_Issue_1_Pages_1-90__.html

Volume 54, Issue 2, Pages 91-186 (February 2007)

Size: 13.0 MB | Format: PDF | Quality: Original preprint

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Volume 54, Issue 3, Pages 187-278 (March 2007)

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Volume 54, Issue 4, Pages 279-376 (April 2007)

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Volume 54, Issue 5, Pages 377-460 (May 2007)

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Volume 54, Issues 6–7, Pages 461-576 (June–July 2007)

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Volume 54, Issue 8, Pages 577-642 (August 2007)

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Volume 54, Issue 9, Pages 643-716 (September 2007)

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Volume 54, Issue 10, Pages 717-790 (October 2007)

Size: 5.3 MB | Format: PDF | Quality: Original preprint
 
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Volume 54, Issue 11, Pages 791-864 (November 2007)

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Volume 54, Issue 12, Pages 865-930 (December 2007)

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Volume 55, Issue 1, Pages 1-112 (January 2008)

Size: 10.0 MB | Format: PDF | Quality: Original preprint
 
http://www.4shared.com/rar/Qnh-ds7o/Volume_55_Issue_1_Pages_1-112_.html

Volume 55, Issue 2, Pages 113-196 (February 2008)

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Volume 55, Issue 3, Pages 197-276 (March 2008)

Size: 8.2 MB | Format: PDF | Quality: Original preprint
 
http://www.4shared.com/rar/XSeYuwit/Volume_55_Issue_3_Pages_197-27.html

Volume 55, Issue 4, Pages 277-332 (April 2008)

Size: 8.3 MB | Format: PDF | Quality: Original preprint
 
http://www.4shared.com/rar/E8LqmWpX/Volume_55_Issue_4_Pages_277-33.html

Volume 55, Issue 5, Pages 333-430 (May 2008)

Size: 12.6 MB | Format: PDF | Quality: Original preprint
 
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Volume 55, Issue 6, Pages 431-568 (June 2008)

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Volume 55, Issues 7–8, Pages 569-700 (July 2008)

Size: 14.8 MB | Format: PDF | Quality: Original preprint
 
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Volume 55, Issue 9, Pages 701-760 (August 2008)

Size: 8.9 MB | Format: PDF | Quality: Original preprint
 
http://www.4shared.com/rar/6QuBYJIQ/Volume_55_Issue_9_Pages_701-76.html
Volume 55, Issue 10, Pages 761-824 (October 2008)

Size: 6.6 MB | Format: PDF | Quality: Original preprint
 
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Volume 55, Issue 11, Pages 825-944 (November 2008)

Size: 16.9 MB | Format: PDF | Quality: Original preprint
 
http://www.4shared.com/rar/MFZd5OC8/Volume_55_Issue_11_Pages_825-9.html

Volume 55, Issue 12, Pages 945-1252 (December 2008)

Size: 43.1 MB | Format: PDF | Quality: Original preprint
 
http://www.4shared.com/rar/6YMtyOa0/Volume_55_Issue_12_Pages_945-1.html

Volume 56, Issue 1, Pages 1-98 (January 2009)

Size: 14.0 MB | Format: PDF | Quality: Original preprint
 
http://www.4shared.com/rar/QIVzpWOX/Volume_56_Issue_1_Pages_1-98__.html

Volume 56, Issue 2, Pages 99-210 (February 2009)

Size: 7.1 MB | Format: PDF | Quality: Original preprint
 
http://www.4shared.com/rar/MoJ9UXrj/Volume_56_Issue_2_Pages_99-210.html

Volume 56, Issue 3, Pages 211-384 (March 2009)

Size: 26.0 MB | Format: PDF | Quality: Original preprint
 
http://www.4shared.com/rar/CE--Aksu/Volume_56_Issue_3_Pages_211-38.html

Volume 56, Issue 4, Pages 385-494 (April 2009)

Size: 8.9 MB | Format: PDF | Quality: Original preprint
 
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Volume 56, Issues 5–6, Pages 495-692 (May–June 2009)

Size: 25.6 MB | Format: PDF | Quality: Original preprint
 
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Volume 56, Issue 7, Pages 693-792 (July 2009)

Size: 13.7 MB | Format: PDF | Quality: Original preprint
 
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Volume 56, Issue 8, Pages 793-896 (August 2009)

Size: 10.1 MB | Format: PDF | Quality: Original preprint
 
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Volume 56, Issue 9, Pages 897-1012 (September 2009)

Size: 17.2 MB | Format: PDF | Quality: Original preprint
 
http://www.4shared.com/rar/fDDZcxFE/Volume_56_Issue_9_Pages_897-10.html

Volume 56, Issue 10, Pages 1013-1068 (October 2009)

Size: 10.5 MB | Format: PDF | Quality: Original preprint
 
http://www.4shared.com/rar/2lc3Yqq6/Volume_56_Issue_10_Pages_1013-.html

Volume 56, Issues 11–12, Pages 1069-1186 (November–December 2009)

Size: 21.9 MB | Format: PDF | Quality: Original preprint
 
http://www.4shared.com/rar/pBbKnMlr/Volume_56_Issues_56_Pages_495-.html

Volume 57, Issue 1, Pages 1-74 (January 2010)

Size: 11.2 MB | Format: PDF | Quality: Original preprint
 
http://www.4shared.com/rar/GuXodsyo/Volume_57_Issue_1_Pages_1-74__.html

Volume 57, Issue 2, Pages 75-240 (February 2010)

Size: 26.0 MB | Format: PDF | Quality: Original preprint
 
http://www.4shared.com/rar/Pkga8KK8/Volume_57_Issue_2_Pages_75-240.html

Volume 57, Issue 3, Pages 241-358 (March 2010)

Size: 20.4 MB | Format: PDF | Quality: Original preprint
 
http://www.4shared.com/rar/Gy936JcS/Volume_57_Issue_3_Pages_241-35.html

Volume 57, Issue 4, Pages 359-470 (April 2010)

Size: 15.5 MB | Format: PDF | Quality: Original preprint
 
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Volume 57, Issue 5, Pages 471-552 (May 2010)

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Volume 57, Issue 6, Pages 553-630 (June 2010)

Size: 5.0 MB | Format: PDF | Quality: Original preprint

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Volume 57, Issue 7, Pages 631-708 (July 2010)

Size: 14.9 MB | Format: PDF | Quality: Original preprint
 
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Volume 57, Issue 8, Pages 709-778 (August 2010)

Size: 5.1 MB | Format: PDF | Quality: Original preprint
 
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Volume 57, Issue 9, Pages 779-878 (September 2010)

Size: 19.2 MB | Format: PDF | Quality: Original preprint
 
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Volume 57, Issue 10, Pages 879-958 (October 2010)

Size: 8.8 MB | Format: PDF | Quality: Original preprint
 
http://www.4shared.com/rar/5d_uQVjO/Volume_57_Issue_10_Pages_879-9.html

Volume 57, Issues 11–12, Pages 959-1066 (November–December 2010)

Size: 15.5 MB | Format: PDF | Quality: Original preprint
 
http://www.4shared.com/rar/Z30jk-gq/Volume_57_Issues_1112_Pages_95.html

Volume 58, Issue 1, Pages 1-134 (January 2011)

Size: 18.5 MB | Format: PDF | Quality: Original preprint
 
http://www.4shared.com/rar/Epkr_7LS/file.html?

Volume 58, Issue 2, Pages 135-228 (February 2011)

Size: 14.7 MB | Format: PDF | Quality: Original preprint
 
http://www.4shared.com/rar/pGsTS-8x/file.html?

Volume 58, Issue 3, Pages 229-280 (March 2011)

Size: 7.8 MB | Format: PDF | Quality: Original preprint
 
http://www.4shared.com/rar/nyskoeuW/file.html?

Volume 58, Issue 4, Pages 281-384 (April 2011)

Size: 14.4 MB | Format: PDF | Quality: Original preprint
 
http://www.4shared.com/rar/88alJqK1/file.html?

Volume 58, Issue 5, Pages 385-452 (May 2011)

Size: 9.4 MB | Format: PDF | Quality: Original preprint
 
http://www.4shared.com/rar/8KQ-wlrI/file.html?

Volume 58, Issue 6, Pages 453-578 (June 2011)

Size: 14.5 MB | Format: PDF | Quality: Original preprint
 
http://www.4shared.com/rar/lvfLN2Qw/file.html?

Volume 58, Issue 7, Pages 579-656 (July 2011)

Size: 6.9 MB | Format: PDF | Quality: Original preprint
 
http://www.4shared.com/rar/c7zbd4HT/file.html?

Volume 58, Issue 8, Pages 657-814 (August 2011)

Size: 21.6 MB | Format: PDF | Quality: Original preprint
 
http://www.4shared.com/rar/j4Qconsa/file.html?

Volume 58, Issue 9, Pages 815-952 (September 2011)

Size: 24.8 MB | Format: PDF | Quality: Original preprint
 
http://www.4shared.com/rar/y95nic1o/file.html?

Volume 58, Issue 10, Pages 953-1012 (October 2011)

Size: 8.5 MB | Format: PDF | Quality: Original preprint
 
http://www.4shared.com/rar/QT0JoHAa/file.html?

Volume 58, Issue 11, Pages 1013-1088 (November 2011)

Size: 8.3 MB | Format: PDF | Quality: Original preprint
 
http://www.4shared.com/rar/hKQsfpgE/file.html?

Volume 58, Issue 12, Pages 1089-1138 (December 2011)

Size: 4.7 MB | Format: PDF | Quality: Original preprint
 
http://www.4shared.com/rar/jFJeHTcf/file.html?

Volume 58, Issue 1, Pages 1-134 (January 2011)

Size: 18.5 MB | Format: PDF | Quality: Original preprint
 
http://www.4shared.com/rar/Epkr_7LS/file.html?

Volume 58, Issue 2, Pages 135-228 (February 2011)

Size: 14.7 MB | Format: PDF | Quality: Original preprint
 
http://www.4shared.com/rar/pGsTS-8x/file.html?

Volume 58, Issue 3, Pages 229-280 (March 2011)

Size: 7.8 MB | Format: PDF | Quality: Original preprint
 
http://www.4shared.com/rar/nyskoeuW/file.html?

Volume 58, Issue 4, Pages 281-384 (April 2011)

Size: 14.4 MB | Format: PDF | Quality: Original preprint
 
http://www.4shared.com/rar/88alJqK1/file.html?

Volume 58, Issue 5, Pages 385-452 (May 2011)

Size: 9.4 MB | Format: PDF | Quality: Original preprint
 
http://www.4shared.com/rar/8KQ-wlrI/file.html?

Volume 58, Issue 6, Pages 453-578 (June 2011)

Size: 14.5 MB | Format: PDF | Quality: Original preprint
 
http://www.4shared.com/rar/lvfLN2Qw/file.html?

Volume 58, Issue 7, Pages 579-656 (July 2011)

Size: 6.9 MB | Format: PDF | Quality: Original preprint
 
http://www.4shared.com/rar/c7zbd4HT/file.html?

Volume 58, Issue 8, Pages 657-814 (August 2011)

Size: 21.6 MB | Format: PDF | Quality: Original preprint
 
http://www.4shared.com/rar/j4Qconsa/file.html?

Volume 58, Issue 9, Pages 815-952 (September 2011)

Size: 24.8 MB | Format: PDF | Quality: Original preprint
 
http://www.4shared.com/rar/y95nic1o/file.html?

Volume 58, Issue 10, Pages 953-1012 (October 2011)

Size: 8.5 MB | Format: PDF | Quality: Original preprint
 
http://www.4shared.com/rar/QT0JoHAa/file.html?

Volume 58, Issue 11, Pages 1013-1088 (November 2011)

Size: 8.3 MB | Format: PDF | Quality: Original preprint
 
http://www.4shared.com/rar/hKQsfpgE/file.html?

Volume 58, Issue 12, Pages 1089-1138 (December 2011)

Size: 4.7 MB | Format: PDF | Quality: Original preprint
 
http://www.4shared.com/rar/jFJeHTcf/file.html?


منبع : آپارات , شرکت نماپرداز رايانه (NPR)
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