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Long-term trends in maximum, minimum and mean annual air temperatures across the Northwestern Himalaya during the twentieth century

机译:二十世纪西北喜马拉雅山的最高,最低和平均每年气温的长期趋势

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The study reveals significant rise in air temperature in the northwest Himalayan (NWH) region by about 1.6pC in the last century, with winters warming at a faster rate. The diurnal temperature range (DTR) has also shown a significantly increasing trend. This appears to be due to rise in both the maximum as well as minimum temperatures, with the maximum increasing much more rapidly. The results are in contrast to the findings in the Alps and Rockies where the minimum temperatures have increased at an elevated rate. Conforming to the global trends, the study confirms episodes of strong warming and cooling in the NWH in the last century. Real warming appears to have started from late-1960s and highest rate of increase was experienced in the last two decades. The study also shows teleconnections between temperatures and an epochal behaviour of the precipitation till late-1960s. These teleconnections seem to have weakened gradually since then and rapidly in the post-1991 period, indicating the waning effect of the natural forcings in this period.
机译:这项研究表明,上个世纪喜马拉雅西北地区的气温显着上升了1.6pC,冬季变暖的速度更快。昼夜温度范围(DTR)也显示出明显的上升趋势。这似乎是由于最高和最低温度的升高,而最高温度的升高要快得多。这个结果与阿尔卑斯山和落基山脉的发现相反,在阿尔卑斯山和落基山脉,最低温度以升高的速率上升。根据全球趋势,该研究证实了上个世纪西北地区强烈的变暖和降温事件。真正的变暖似乎始于1960年代后期,并且在过去的20年中经历了最高的增速。该研究还表明,直到1960年代后期,温度与降水的时代行为之间存在遥相关。从那时起,这些遥相关似乎逐渐减弱,并在1991年后时期迅速减弱,这表明该时期自然强迫的作用正在减弱。

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