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首页> 外文期刊>Open Journal of Marine Science >The Trend of Changes in Surface Wind in the Indian Ocean, in the Period from 1981 to 2015, Using Reanalysis Data, NCEP/NCAR
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The Trend of Changes in Surface Wind in the Indian Ocean, in the Period from 1981 to 2015, Using Reanalysis Data, NCEP/NCAR

机译:印度洋在印度洋的变化趋势,从1981年到2015年,使用重新分析数据,NCEP / NCAR

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Knowing the pattern of surface winds on the seas and oceans and how it changes over time is of great importance. In this research, the monthly surface wind fields on the Indian Ocean have been studied and analyzed for a 35-year period (1981-2015), using NCEP/NCAR data reanalysis. The results show that transition from cold to warm pattern happens in May and that the summer monsoon pattern begins in June and continues until August. The wind speed pattern tends to the winter monsoon from November on. The maximum average wind speed in June is 13 m/s and its minimum is 2 m/s in October. Direction of prevailing winds is the southwest in the summer. The highest wind speed happens in the latitude of 10 - 15 degrees. Analysis of the wind distribution shows that the wind speed of 2 - 5 m/s happens in about 60% of the cases. There is probability of blowing 0.5 - 4 m/s wind for all months; but this probability is higher in the autumn (October and November) than that in the summer (July and August). Probability of the monthly over 5 m/s winds shows a definitely opposite distribution; that is, wind speed in July and August is higher than that in October. A long-term survey on the speed of surface water wind and sea surface temperature shows an opposite changing trend in wind speed and sea surface temperature during a 55-year statistical period. Wind speed reduced, while the sea surface temperature was increasing. The wind speed gradient in the upper levels of atmosphere graph has been increasing; this phenomenon confirms the effects of global warming and ocean warming on the monsoon system patterns in the Indian Ocean. Keywords North
机译:了解海洋和海洋表面风的模式以及随时间变化的变化是非常重要的。在这项研究中,使用NCEP / NCAR数据再分析,研究并分析了印度洋上的每月地表风田,并分析了35年(1981-2015)。结果表明,5月份从寒冷到温暖模式的过渡发生,夏季季风模式在6月开始,持续到8月。风速模式从11月开始往往冬季季风。 6月的最大平均风速为13米/秒,10月份最低为2米/秒。盛行风的方向是夏季西南部。最高的风速发生在10 - 15度的纬度。对风分配的分析表明,在大约60%的情况下发生了2-5米/秒的风速。所有月份都有0.5 - 4米/米风的概率;但这种概率在秋季(10月和11月)比夏天(7月和8月)更高。每月超过5米/米风的概率显示出绝对相反的分布;也就是说,7月和8月的风速高于10月份。关于地表水风速和海面温度的长期调查显示了55年统计期间风速和海面温度的相反变化趋势。风速减少,而海表面温度越来越大。大气图的上层的风速梯度一直在增加;这种现象证实了全球变暖和海洋变暖对印度洋的季风系统模式的影响。关键词北

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