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Climate change features along the Brahmaputra Valley in the past 26 years and possible causes

机译:过去26年雅鲁藏布江沿岸的气候变化特征及其可能原因

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Through analyzing the changes of averaged temperature and precipitation along the Brahmaputra Valley from 1980 to 2005, and investigating the correlation between atmospheric circulation indices and these changes, the respondence of the Brahmaputra Valley to the global warming had been analyzed in this paper. It is found that the Brahmaputra Valley climate became warmer and wetter from 1980 to 2005, and the change magnitude is higher than that over the whole Tibetan Plateau. Therefore, the respondence of the Brahmaputra valley to the global warming is more evident than that of the whole plateau during the period. The relationship between atmospheric circulation indices and the regional climate change is significant. When North Atlantic Oscillation index is higher in summer, the climate of the Brahmaputra Valley becomes warmer and dryer; vice versa. When South Oscillation index is higher, it becomes warmer and wetter; vice versa.Worthy of note, the results in this study only emphasize some evidence of change in temperature and precipitation over the Brahmaputra Valley during 1980–2005.
机译:通过分析布拉马普特拉河谷1980年至2005年的平均温度和降水变化,并调查大气环流指数与这些变化之间的相关性,分析了布拉马普特拉河谷对全球变暖的响应。研究发现,1980年至2005年,雅鲁藏布江谷的气候变暖和湿润,其变化幅度高于整个青藏高原。因此,在此期间,雅鲁藏布江谷对全球变暖的响应比整个高原的响应更明显。大气环流指数与区域气候变化之间的关系很重要。夏季北大西洋涛动指数较高时,雅鲁藏布江谷的气候变暖和干燥。反之亦然。当南方涛动指数较高时,它将变暖和变湿;反之亦然。值得一提的是,这项研究的结果仅强调了1980-2005年间布拉马普特拉谷地温度和降水变化的一些证据。

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