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Change trends of temperature and precipitation in the Loess Plateau Region of China, 1961-2010

机译:黄土高原地区1961-2010年温度和降水变化趋势

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摘要

The Loess Plateau is the most severe soil and water loss area in the world. The changing trencds of annual mean temperature and annual precipitation over the last 50 years in the Loess Plateau Region (LPR) are investigated using observed time series from all available stations. The trends are assessed for both the entire LPR and its five integrated management divisions using the gridded data. It is shown that the region-sveraged annual mean temperature has significantly increased over the last 50 years (1.91 ℃/S0yr), whereas the region-averaged annual precipitation shows a non-significant negative trend ( - 29.11 mm/50 yr) Spatially, there is an enhanced warming gradient but an obvious drying to weak wetting gradient from the southeast to the northwest across the region. On divisional scales, a significant warming trend is detected for all the divisions. A significant drying trend and a nearly significant drying trend are found for the first and second divisioons, respectively, and a non-significant positive trend for other divisions. Therefore the region can be divided into, e southeast warming and drying sub-region (SESR) and the northwest warming and weak wetting sub-ragion. 'NWSR). Further analysis shows that the SESR has a significant warming trend (1.71 ℃/50 yr) and a significant deying trend (-47.62 mm/50 yr), and the NWSR has a significant warming trend (2.25 ℃/50 yr) but a non-significat; wetting trend (15.20 mm/50 yr). These results may have important implication in addressing the challergs of climate change in terms of the integrated management of the LPR.
机译:黄土高原是世界上最严重的水土流失地区。黄土高原地区(LPR)过去50年的年平均温度和年降水量的变化趋势是使用从所有可用台站观测到的时间序列进行调查的。使用网格数据对整个LPR及其五个集成管理部门的趋势进行评估。结果表明,过去50年(1.91℃/ S0yr),该地区的年平均气温显着升高,而该地区的年平均降水量却呈现出不显着的负趋势(-29.11 mm / 50 yr)。在整个区域中,从东南到西北,变暖梯度增加,但明显变干而变弱。在分区范围内,所有分区的升温趋势都很大。第一个和第二个除数分别发现显着的干燥趋势和近乎显着的干燥趋势,而其他部门则没有显着的正趋势。因此,该区域可分为东南暖化和干燥子区域(SESR)和西北暖化和弱湿子区域。 'NWSR)。进一步的分析表明,SESR的变暖趋势很明显(1.71℃/ 50 yr),并且有明显的变暗趋势(-47.62 mm / 50 yr),NWSR的变暖趋势很明显(2.25℃/ 50 yr),但是没有变暖趋势。 -重要润湿趋势(15.20 mm / 50年)。这些结果可能在解决LPR的综合管理方面对应对气候变化挑战具有重要意义。

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