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Atmospheric circulation influence on temperature and precipitation individual and compound daily extreme events: Spatial variability and trends over southern South America

机译:大气循环对温度和降水个体的影响和复合日期极端事件:南美洲南部的空间变异性和趋势

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Southern South America (SSA) is an extended region where temperature and precipitation daily extreme events have several impacts on the different socio-economic activities. In this work, their individual and compound occurrence over SSA and their association with atmospheric circulation were studied during 1979–2015, using meteorological stations and the CPC gridded dataset. Results were generally in good agreement between both datasets. The occurrence of a warm night (minimum temperature exceeding the 90th percentile) or a cold day (maximum temperature below the 10th percentile) significantly increases the probability of heavy precipitation (daily precipitation exceeding the 75th percentile) in southern Chile and southeastern South America. These compound events were regionally conditioned by specific circulation types. In addition, both individual and compound extremes showed trends in the different sub-regions. On one hand, heavy precipitation exhibited a significant increase over central-eastern Argentina and Uruguay, northeastern Argentina and southern Brazil during the warm season, and a significant decrease in central and southern Chile during the cold season. On the other hand, warm (cold) extremes generally presented significant upward (downward) trends. Compound events showed significant positive trends for selected regions, in some cases coincident with trends in individual extremes. Changes in the frequency of circulation patterns were found to partly influence some of these trends, like the increases in heavy precipitation and warm extremes during the warm season.
机译:南美洲南美(SSA)是一个扩展的地区,温度和降水日常极端事件对不同的社会经济活动有几项影响。在这项工作中,在1979-2015期间,使用气象站和CPC网格数据集在1979 - 2015年期间研究了它们的个人和复合事件及其与大气循环的关联。结果通常在两个数据集之间吻合良好。温暖的夜晚(最低温度超过第90百分位数)或寒冷的日子(最高温度低于第10位)显着提高了智利南部和东南美国东南部的重度降水(每日降水超过第75百分位数)的可能性。这些复合事件通过特定循环类型区域调节。此外,个人和复合极端都显示出不同子区域的趋势。一方面,在温暖的季节期间,大量的沉淀,在中央东部阿根廷和乌拉圭,东北部和巴西南部,智利中央和南部的大幅下降。另一方面,温暖(冷)极端通常呈现出显着的向上(向下)趋势。复合事件显示出选定地区的显着正趋势,在某些情况下与个体极端趋势一致。发现循环模式的频率变化部分地影响了这些趋势的一些趋势,就像在温暖季节的重度降水和暖温度的增加一样。

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