西部扰动的频率增加和季节延长与副热带喷流强度增加和北移延迟有关

Kieran M. R. Hunt
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引用次数: 0

摘要

摘要西部扰动(WDs)是沿副热带喷流移动的气旋风暴,在冬季为兴都库什山脉、喀喇昆仑山脉和喜马拉雅山脉西部带来大部分季节性降水和极端降水。它们是该地区水安全的重要组成部分。虽然降雨通常在冬季最为常见,但也会与夏季季风相互作用,导致灾难性后果。这种情况似乎发生得越来越频繁,伴随着冬季的日益严酷,人们现在开始询问气候变化如何影响夏季和冬季的降水频率和强度。对之前 17 项评估 WD 频率趋势的研究进行分析后发现,人们并没有达成共识,至少部分原因是这些研究对不同地区、季节和时间段的趋势进行了量化。本研究采用了一种更稳健的方法,利用从欧洲中期天气预报中心(ECMWF)70 年再分析(ERA5)数据中提取的轨迹目录,按地区和月份量化了 WD 频率和强度的趋势。在过去 70 年中,喜马拉雅西部和中部以及兴都库什山脉的冬季 WD 明显增加。这一趋势归因于副热带喷流的加强。WD 季节也明显延长,WD 在 5 月、6 月和 7 月变得更为常见,而这些月份以前很少出现 WD。例如,在过去 20 年中,6 月份出现 WD 的频率是前 50 年的两倍。这要归因于副热带喷流的延迟北退,而历史上这种情况都发生在夏季季风开始之前。最重要的影响是,"季风性 "WD 的频率正在显著增加,因此,由于气候变化,像 2013 年北阿坎德邦洪水和 2023 年印度北部洪水这样的灾难性事件正在变得更加频繁。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Increasing frequency and lengthening season of western disturbances are linked to increasing strength and delayed northward migration of the subtropical jet
Abstract. Western disturbances (WDs) are cyclonic storms that travel along the subtropical jet, bringing the majority of seasonal and extreme precipitation to the Hindu Kush, Karakoram, and western Himalaya in the winter months. They are a vital component of the region's water security. Although typically most common in the winter, WDs can also interact with the summer monsoon, leading to catastrophic consequences. These seem to be happening more frequently, and along with increasingly harsh winter seasons, questions are now being asked about how climate change is affecting WD frequency and intensity in both summer and winter seasons. An analysis of 17 previous studies assessing trends in WD frequency revealed no consensus, at least in part because they quantified trends in different regions, seasons, and time periods. In this study, a more robust approach is used, quantifying trends in WD frequency and intensity by region and month using a track catalogue derived from 70 years of European Centre for Medium-Range Weather Forecasts (ECMWF) reanalysis (ERA5) data. Winter WDs have increased significantly over the western and central Himalaya and the Hindu Kush in the last 70 years. This trend is attributed to a strengthening of the subtropical jet. The WD season has also significantly lengthened with WDs becoming far more common in May, June, and July, months where they were previously rare. For example, WDs have been twice as common in June in the last 20 years than during the previous 50. This is attributed to a delayed northward retreat of the subtropical jet, which historically has occurred before the onset of the summer monsoon. The most important implication is that the frequency of “monsoonal” WDs is increasing significantly, and therefore, due to climate change, catastrophic events like the 2013 Uttarakhand floods and the 2023 north India floods are becoming much more frequent.
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