Identifying hot spots of long-duration extreme climate events in the northwest arid region of China and implications for glaciers and runoff

Pub Date : 2022-12-01 DOI:10.1016/j.rcar.2023.02.004
ShaoPing Wang , YongJian Ding , FengQing Jiang , XiaoDong Wu , Jie Xue
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引用次数: 1

Abstract

China's Northwest Arid Region (NAR), with dry and cold climate conditions and glaciers widely developed in the high mountains, provides vital water resources for Asia. The consecutive cold, warm, dry and wet days have much higher impacts on the water cycle process in this region than extreme temperature and precipitation events with short durations but high intensities. Parametric and nonparametric trend analysis methods widely used in climatology and hydrology are employed to identify the temporal and spatial features of the changes in the consecutive cold, warm, dry and wet days in the NAR based on China's 0.5° × 0.5° meteorological grid datasets of daily temperature and precipitation from 1961 to 2018. This study found that (1) the consecutive cold days (Cold Spell Duration Indicator, CSDI), and the consecutive dry days (CDD) decreased, while the consecutive warm days (Warm Spell Duration Indicator, WSDI), and the consecutive wet days (CWD) increased from 1961 to 2018, (2) and the eastern Kunlun Mountains were the hot spots where all of these consecutive climate indices changed significantly, (3) and the changes in these consecutive climate indices were highly correlated with the rise in the Global Mean Land/Ocean Temperature Index. The results indicated that winters tended to warmer and dryer and summer became hotter and wetter during 1961–2018 in the NAR under the global warming, which can lead to the sustained glacier retreat and the increase in summer runoff in this region, and the eastern Kunlun Mountains are the area where could face high risks of water scarcity and floods if the changes in these climate indices continue in the future. Given the vulnerability of the socio-economic systems in the NAR to a water shortage and floods, it is most crucial to improve the strategies of water resources management, disaster prevention and risk management for this region under climate change.

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中国西北干旱区长时间极端气候事件热点识别及其对冰川和径流的影响
中国西北干旱区气候干燥寒冷,高山冰川广泛发育,为亚洲提供了重要的水资源。连续冷暖干湿日对该地区水循环过程的影响远大于持续时间短但强度大的极端温度和降水事件。基于1961 - 2018年中国0.5°× 0.5°气象格点逐日气温和降水数据集,采用气体学和水文学中常用的参数和非参数趋势分析方法,识别了全国气象数据中心连续冷暖干湿日数变化的时空特征。研究发现:(1)1961 - 2018年连续冷日数(cold Spell Duration Indicator, CSDI)和连续干日数(CDD)减少,连续暖日数(warm Spell Duration Indicator, WSDI)和连续湿日数(CWD)增加,(2)东部昆仑山脉是上述连续气候指标变化显著的热点地区;(3)连续气候指数的变化与全球平均海陆温度指数的上升高度相关。结果表明:在全球变暖的背景下,1961—2018年NAR冬季偏暖偏干,夏季偏热偏湿,导致该地区冰川持续退缩,夏季径流量增加,如果这些气候指标持续变化,未来昆仑山东部地区将面临水资源短缺和洪涝灾害的高风险。鉴于该地区的社会经济系统对水资源短缺和洪水的脆弱性,在气候变化下,改善该地区的水资源管理、灾害预防和风险管理战略至关重要。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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