The polar front forms where the polar easterlies and the prevailing westerlies converge. |
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The influence of prevailing westerlies is responsible for bringing air from the interior of the North American continent to New Brunswick. |
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Orographic lifting causes the ecodistrict to intercept moisture from the prevailing westerlies, bringing relatively high levels of precipitation. |
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Net precipitation is high near the Equator and also in the belts of the prevailing westerlies where there is frequent storm activity. |
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There are four main belts: the doldrums, the horse latitude belts, the trade wind belts, and the belts of the prevailing westerlies. |
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Temperate zones, such as Europe, get more of their rain in the winter from the effect of low-pressure zones coming in from the Atlantic driven by the prevailing westerlies. |
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Best time to go As we rely on prevailing westerlies to fill in the snow to the back bowls, February and March are usually better than January. |
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Europe lies mainly in the temperate climate zones, being subjected to prevailing westerlies. |
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These upper-air, prevailing westerlies encircle the globe in a wave-like pattern, undulating north and south as they flow along the latitude belt. |
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Wind patterns must have included strong polar easterlies at high northern latitudes, prevailing westerlies at midlatitudes, and northeast trade winds in the tropics. |
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The prevailing westerlies are north and south of the horse latitude belts. |
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The greater part of Canada lies in the path of the prevailing westerlies. |
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The relative warmth of the Gulf Stream affects air temperatures all the way across the Atlantic, and prevailing westerlies extend the warming effect deep into northern Europe. |
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Thus, they frequently move clockwise around the periphery of the North Atlantic high-pressure belt and into the prevailing westerlies, often ending up in the Icelandic area. |
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The prevailing westerlies in these zones blow strongest in winter. |
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Prevailing westerlies occur between the polar easterlies and trade winds. |
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