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首页> 外文期刊>International Journal of Climatology: A Journal of the Royal Meteorological Society >Comprehensive analysis of the climate variability in the eastern Mediterranean. Part I: map-pattern classification
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Comprehensive analysis of the climate variability in the eastern Mediterranean. Part I: map-pattern classification

机译:地中海东部气候变异性的综合分析。第一部分:地图模式分类

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This paper provides an extended study of the dominant daily circulation patterns governing the climate variability in the eastern Mediterranean. The methodology adopted to determine the circulation patterns is based on combined analysis of the spatial and temporal variation of rotated principal components of sea-level pressure. A catalogue of characteristic seasonal composites is presented and discussed. It is found that, during winter and spring, large scale features situated in northern Europe affect the atmospheric circulation over the domain of study, whereas the Atlantic (Azores) anticyclone and the Asian Thermal Low define most of the observed circulation types in summer. In autumn, the area exhibits a rapid transition from the warm to cold season showing climatic features from both extreme seasons. Similarities between winter and spring/autumn patterns are detected and correlation analyses are employed between their spatial patterns to reveal that similar circulation patterns occur amongst the three seasons, which usually appear more pronounced during winter. Frequencies and trends of the proposed circulation types are examined for each season. A linear trend analysis for the overall period (1958-2000) exhibits a significant increase in the anticyclonic types particularly in winter. With respect to the cyclonic types, statistically significant negative trends have been found in all seasons especially for types associated with depressional activity in central the Mediterranean. Copyright (C) 2007 Royal Meteorological Society
机译:本文提供了关于控制地中海东部气候变化的主要日循环模式的扩展研究。确定循环模式所采用的方法是基于对海平面压力旋转主分量的时空变化的综合分析。介绍并讨论了典型的季节性复合材料目录。结果发现,在冬季和春季,位于北欧的大规模特征影响了研究范围内的大气环流,而在夏季,大西洋(亚速尔群岛)的反气旋和亚洲热低层定义了大多数观测到的环流类型。在秋天,该地区表现出从暖季到冷季的快速过渡,显示了两个极端季节的气候特征。探测到冬季和春季/秋季模式之间的相似性,并在它们的空间模式之间进行相关分析,以揭示三个季节之间出现相似的循环模式,通常在冬季更为明显。针对每个季节检查建议的流通类型的频率和趋势。整个时期(1958-2000年)的线性趋势分析显示,尤其在冬季,反气旋类型显着增加。关于气旋类型,在所有季节都发现了统计学上显着的负趋势,尤其是与地中海中部与抑郁活动有关的类型。皇家气象学会(C)2007

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