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Changes in surface wind directions in Estonia during 1966-2008 and their relationships with large-scale atmospheric circulation

机译:1966-2008年爱沙尼亚地面风向的变化及其与大规模大气环流的关系

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摘要

Changes in the percentages of eight main surface wind directions at 14 meteorological stations in Estonia, Northeast Europe, were studied during 1966-2008. Long-term changes in wind directions are related to variations in the large-scale atmospheric circulation but partly also to changes in the surroundings of the stations and in wind obstacles. Significant alterations in wind directions were determined, and found to be the strongest in the winter season. The percentages of W and SW winds have clear positive trends, while SE, E and NE winds are characterized by negative tendencies in winter. In conclusion, wind directions have probably been shifted from east to west. Differences in trends between the stations are explained by changes in wind obstacles around the stations. The trends in wind roses in Estonia were caused by the intensification of the westerly circulation over the Atlantic/European sector during the winter season.
机译:在1966-2008年期间,研究了东北爱沙尼亚14个气象站的8个主要地面风向百分比的变化。风向的长期变化与大规模大气环流的变化有关,但也部分与气象站周围环境和风障的变化有关。确定了风向的重大变化,发现是冬季最强烈的变化。西南风的百分比具有明显的正趋势,而东南风,东风和东北风的特征是冬季为负趋势。总之,风向可能已从东移到西。站点之间趋势的差异可以通过站点周围的风障变化来解释。爱沙尼亚风玫瑰的趋势是由于冬季冬季大西洋/欧洲地区西风环流的加剧。

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