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Spatial and temporal variations in air temperature and precipitation in the Chinese Himalayas during the 1971-2007

机译:1971-2007年中国喜马拉雅山气温和降水的时空变化

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摘要

The Chinese Himalayas (CH) is highly sensitive to global climate change. The analyses of monthly mean air temperature and monthly precipitation data during the 1971-2007 from 24 meteorological stations show a significant increase of 0.31°C per decade or about 1.15°C for annual mean air temperature over the entire region. The temperature rise occurs primarily during the period of 1991-2007, up to 0.73°C per decade. Climate warming is characterized by all-year temperature increase in particular during winters with the maximum value of 0.38°C per decade during the 1971-2007, up to 1.24°C per decade during 1991-2007. Distributions of annual temperature trends show significant south-to-north, low-to-high and east-to-west warming trends to increase with the latitude and elevation while to decrease with the longitude in the CH, respectively. Annual precipitation increases, but not significantly during the 1971-2007. Seasonal precipitation has no significant trend during the same period, either. Spatial discrepancy of the variations in precipitation is particularly great. It is evident that the climate was significantly warming and drying in the western CH over the past 37 years.
机译:中国喜马拉雅山(CH)对全球气候变化高度敏感。对1971-2007年间24个气象站的月平均气温和月降水量数据进行的分析显示,每十年显着增加0.31°C,或者整个区域的年平均气温约1.15°C。温度上升主要发生在1991-2007年期间,每十年最高上升0.73°C。气候变暖的特点是全年温度都在升高,尤其是在冬季,1971-2007年期间每十年的最高温度为0.38°C,1991-2007年期间每十年的最高温度为1.24°C。年气温趋势的分布表明,南半球,北半球,北半球,北半球,北半球,北半球,北半球,北半球,北半球,北半球,北半球,北半球,北半球,北半球,北半球和北半球都有明显的变暖趋势。年降水量增加,但在1971-2007年期间并不显着。同期,季节性降水也无明显趋势。降水变化的空间差异特别大。显然,在过去的37年中,CH西部的气候明显变暖和干燥。

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