黄土高原夏季土壤水分干旱的短持续期和长持续期类型及其遥相关关系

IF 4.5 2区 地球科学 Q1 METEOROLOGY & ATMOSPHERIC SCIENCES
Jialan Hu , Shuangshuang Li , Xianfeng Liu , Guangyao Gao
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引用次数: 0

摘要

土壤水分干旱对植被生长和水资源具有破坏性影响。基于事件的干旱过程建模可以为更好地理解中国季风和黄土临界带不同类型土壤水分干旱对大尺度遥相关的响应提供途径。基于SMCI1.0日土壤水分数据,发现2000 - 2020年黄土高原夏季土壤水分干旱加剧,夏季标准化土壤水分指数(SSMI)年- 1下降1.5%。根据事件的持续时间和空间覆盖度,将黄土高原12个夏季土壤水分干旱事件分为短持续期(6 ~ 14 d)和长持续期(≥15 d)两类,并进一步讨论了它们之间的大尺度遥相关关系。有趣的是,我们发现夏季短(长)期土壤水分干旱受到波列(阻塞)环流异常的影响。夏季土壤水分干旱以欧亚大陆上空东向的“−+−+”波列爆发,其主要原因是北大西洋的三极海温模态和南亚高压减弱并西移。这种结构导致黄土高原水汽亏缺,有利于黄土高原夏季土壤水分干旱时间的缩短。对于持续时间较长的夏季土壤水分干旱,持续温暖的热带大西洋和北海-波罗的海有利于“+−+”波列,使冷空气南下运动减弱,水汽亏缺持续时间较长,水汽亏缺伴随下行盛行,为夏季土壤水分亏缺持续时间较长和增强提供了有利条件。揭示与不同类型土壤水分干旱事件相关的大尺度遥相关不仅可以提供干旱预警信息,还可以为黄土高原或欧亚其他旱地的植被恢复工程提供科学指导。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Identifying the short-duration and long-duration types of summer soil moisture drought on the Loess plateau and their teleconnections

Identifying the short-duration and long-duration types of summer soil moisture drought on the Loess plateau and their teleconnections
Soil moisture drought poses a destructive effect on vegetation growth and water resource. Modeling event-based drought processes could serve as a pathway for better understanding how different types of soil moisture drought responds to larger-scale teleconnections in the monsoon and loess critical zone of China. Based on the daily soil moisture dataset named SMCI1.0 at top 1 m, we found that the Loess Plateau witnessed an aggravated summer soil moisture drought, with summer standardized soil moisture index (SSMI) decreasing by 1.5 % year−1 from 2000 to 2020. According to the durations and spatial coverage of events, we classified 12 summer soil moisture drought events occurring on the Loess Plateau into short-duration (6–14 days) and long-duration (≥15 days) types, and further discussed their different large-scale teleconnections. Interestingly, we found the short-duration (long-duration) summer soil moisture drought was influenced by wave train (blocking) circulation anomalies. The short-duration summer soil moisture drought broke out with an eastward “− + − +” wave train over Eurasia, which was mainly attributed to a tripolar sea surface temperature (SST) mode over the North Atlantic and weakened South Asian high (SAH) with westward shift. Such a structure resulted in water vapor deficit of Loess Plateau, and thus favored shorter summer soil moisture drought on the Loess Plateau. For the long-duration summer soil moisture drought, consistently warm tropical Atlantic and North Sea-Baltic Sea favored the “+ − +” wave train, weaking the southward movement of cold air and maintaining prolonged water vapor deficit accompanied by downward prevails, which consequently provided a favorable condition for more long-lasting and enhanced summer soil moisture deficit. Insights into the large-scale teleconnections related to the different types of soil moisture drought event not only can provide drought early warning information, but also offer a scientific guidance for revegetation projects on the Loess Plateau or other Eurasian drylands.
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来源期刊
Atmospheric Research
Atmospheric Research 地学-气象与大气科学
CiteScore
9.40
自引率
10.90%
发文量
460
审稿时长
47 days
期刊介绍: The journal publishes scientific papers (research papers, review articles, letters and notes) dealing with the part of the atmosphere where meteorological events occur. Attention is given to all processes extending from the earth surface to the tropopause, but special emphasis continues to be devoted to the physics of clouds, mesoscale meteorology and air pollution, i.e. atmospheric aerosols; microphysical processes; cloud dynamics and thermodynamics; numerical simulation, climatology, climate change and weather modification.
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