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TROUBLED WATERS - Whale and Dolphin Conservation Society

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chance of fog decreases from 15 to 5 per cent. In the following months to November there is no clear<br />

trend. In December, the probability of precipitation is 24 per cent. These results indicate that March<br />

has the highest chance of precipitation of all the whaling months. The probability of fog is highly<br />

variable in the winter, but from September onwards, the probability of fog increases from 3 per cent to<br />

around 15 per cent in December <strong>and</strong> January. Thus, in the period when the probability of precipitation<br />

is low, the probability of fog is relatively high. So if the issue of reduced visibility is considered, fogrelated<br />

problems add to those caused by precipitation in these months. How the whalers respond to fog<br />

or precipitation is unclear, <strong>and</strong> it would be of great value if more information was made available by the<br />

whalers to help underst<strong>and</strong> how these weather states affect the efficiency of whale killing.<br />

Wind speed <strong>and</strong> wave height<br />

The average wind speed, regardless of its direction, increases from 7.4 ms-1 (a moderate breeze) in<br />

January to 9.3 ms-1 (fresh breeze) in March. However, the wind speed is highly variable from April<br />

until October, with the highest variation in the months with the highest averages. These are September<br />

<strong>and</strong> October (10.5 ms-1; fresh breeze). Thereafter the wind speed reduces to 7.7 ms-1 in December.<br />

Given the variation, probabilities of wind speeds higher than 11.2 ms-1 (strong breeze <strong>and</strong> higher) in<br />

March or November, or 14.3 ms-1 (moderate gale <strong>and</strong> higher) in October are significant (10, 13 <strong>and</strong><br />

20 per cent respectively).<br />

The average height of the waves (calculated from the upper third of all wave heights, known as<br />

‘significant wave height’, see also www.oceanweather.com ) <strong>and</strong> the time between reoccurrences of the<br />

most violent <strong>and</strong> energetic waves (known as ‘Tpeak’) is estimated at one location: 67.5° S <strong>and</strong> 180° W.<br />

This has been done using the GROW model of Oceanweather Inc. <strong>and</strong> is based on the years 1970 until<br />

2001. The average significant wave height tends to increase from 2.2 to 3.4 metres between January<br />

<strong>and</strong> March <strong>and</strong> tends to remain relatively high until June with an average wave height of 3.2 metres.<br />

The height is not known for the following months, but averages 1.9 metres in December. The missing<br />

values are for months in <strong>and</strong> after the winter, when the ice covers the sea. The model excludes data in<br />

these cases. The Tpeak seems to follow the same trend as the wave height, starting with around 10.5<br />

seconds in December <strong>and</strong> January <strong>and</strong> increasing thereafter to about 11.5 seconds in the period April<br />

to June.<br />

The wind increases from January until March, but becomes more variable thereafter. This together with<br />

the growing percentage of ice in the area, blocking wave formation after March, may explain why the<br />

highest waves are found in March before the significant formation of sea ice. It can, therefore, be<br />

postulated that March may be one of the most severe months (in terms of adverse weather conditions)<br />

in which to perform whaling operations in the research area.<br />

Ship motions in March <strong>and</strong> December at an Antarctic whaling ground<br />

Ship motions have been calculated using the SHIPMO computer programme of the Maritime Research<br />

Institute in the Netherl<strong>and</strong>s (Anon 2002). The ship used for these calculations was similar to the<br />

Japanese whale catching vessel Toshi Maru No.25. A sailing speed of 6 knots, head seas coming in at 30<br />

degrees <strong>and</strong> local sea depth of 1,000 metres were used in the model. The model was run for estimated<br />

sea conditions during March <strong>and</strong> December, as described above. The motions considered were, the<br />

sway (from left to right), heave (up <strong>and</strong> down) <strong>and</strong> surge (forward <strong>and</strong> backward), as would be<br />

experienced at the level of the harpoon on top of the bow. Table 1 provides the results for these<br />

different motions in December <strong>and</strong> March.<br />

WEATHER, SEA CONDITION AND SHIP MOTIONS AFFECTING ACCURACY IN WHALING<br />

65

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