Teleconnections of Atmospheric Circulations to Meteorological Drought in the Lancang-Mekong River Basin

Atmosphere Pub Date : 2024-01-10 DOI:10.3390/atmos15010089
Lei Fan, Yi Wang, Chenglin Cao, Wen Chen
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Abstract

The Lancang-Mekong River Basin (LMRB) is one of the major transboundary basins globally, facing ongoing challenges due to flood and drought disasters. Particularly in the past two decades, the basin has experienced an increased frequency of meteorological drought events, posing serious threats to the local socio-economic structures and ecological systems. Thus, this study aimed to analyze the meteorological drought characteristics in the LMRB and identify the impact and correlation of atmospheric circulation on the meteorological drought in the basin. Specifically, the different levels of meteorological drought events were defined using the Run Theory based on the seasonal and annual SPEI from 1980 to 2018. The time lag correlation between meteorological drought events and the EI Nino-Southern Oscillation (ENSO), Arctic Oscillation (AO), North Atlantic Oscillation (NAO), and Pacific Decadal Oscillation (PDO), were analyzed in the LMRB. Our results indicated that, from a temporal perspective, the period from November to April of the following year was particularly prone to meteorological droughts in the basin. In terms of spatial distribution, the primary agricultural regions within the basin, including Thailand, Eastern Cambodia, and Vietnam, were highly susceptible to meteorological droughts. Further analysis revealed a teleconnection between drought events in the LMRB and atmospheric circulation factors. The sensitivity of the basin’s drought timing to its response decreased in the order of the ENSO > AO > NAO > PDO. In general, the ENSO had the most substantial influence on drought events in the basin, with the strongest response relationship, while the upper reaches of the basin displayed the most significant response to the AO; the occurrence and progression of meteorological droughts in this area synchronized with the AO. These findings enhance our understanding of drought-prone areas in the LMRB, including the meteorological factors and driving mechanisms involved. This information is valuable for effectively mitigating and managing drought risks in the region.
大气环流与澜沧江-湄公河流域气象干旱的远程联系
澜沧江-湄公河流域(LMRB)是全球主要跨境流域之一,面临着洪水和干旱灾害带来的持续挑战。特别是近二十年来,流域内气象干旱事件频发,对当地的社会经济结构和生态系统构成了严重威胁。因此,本研究旨在分析河套地区的气象干旱特征,明确大气环流对流域气象干旱的影响及相关性。具体而言,根据1980年至2018年的季节和年度SPEI,利用运行理论定义了不同等级的气象干旱事件。在 LMRB 中分析了气象干旱事件与厄尔尼诺-南方涛动(ENSO)、北极涛动(AO)、北大西洋涛动(NAO)和太平洋十年涛动(PDO)之间的时滞相关性。结果表明,从时间角度看,11 月至次年 4 月是该流域气象干旱的多发期。从空间分布来看,盆地内的主要农业区,包括泰国、柬埔寨东部和越南,极易受到气象干旱的影响。进一步的分析表明,低纬度河谷盆地的干旱事件与大气环流因素之间存在着遥相呼应的关系。该流域的干旱时间对其反应的敏感性按照 ENSO > AO > NAO > PDO 的顺序递减。总体而言,厄尔尼诺/南方涛动对流域干旱事件的影响最大,响应关系最强,而流域上游对涛动的响应最为显著;该地区气象干旱的发生和发展与涛动同步。这些发现加深了我们对低纬度和中纬度地区干旱易发区的了解,包括相关的气象因素和驱动机制。这些信息对于有效缓解和管理该地区的干旱风险非常有价值。
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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