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Characteristics of spatial and temporal variations of monthly mean surface air temperature over Qinghai-Tibet Plateau

机译:青藏高原月平均气温的时空变化特征

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摘要

The recorded meteorological data of monthly mean surface air temperature from 72 meteorological stations over the Qinghai-Tibet Plateau in the period of 1960–2003 have been analyzed by using Empirical Orthogonal Function (EOF) method, to understand the detailed features of its temporal and spatial variations. The results show that there was a high consistency of the monthly mean surface air temperature, with a secondarily different variation between the north and the south of the plateau. Warming trend has existed at all stations since the 1960s, while the warming rates were different in various zones. The source regions of big rivers had intense warming tendency. June, November and December were the top three fast-warming months since the 1960s; while April, July and September presented dramatic warming tendency during the last decade.
机译:运用经验正交函数(EOF)方法对青藏高原72个气象站1960-2003年的月平均气温记录数据进行了分析,以了解其时空特征。变化。结果表明,每月平均地面气温具有较高的一致性,高原北部和南部之间的变化次之。自1960年代以来,所有气象站都存在变暖趋势,而各​​个地区的变暖率却有所不同。大河源区变暖趋势强烈。 6月,11月和12月是自1960年代以来最快速的三个月。在过去的十年中,四月,七月和九月呈现出剧烈的变暖趋势。

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