Analysis of drought characteristics and causes in Yunnan Province in the last 60 years (1961-2020)

IF 3.1 3区 地球科学 Q2 METEOROLOGY & ATMOSPHERIC SCIENCES
Tianqing Lan, Xiaodong Yan
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引用次数: 0

Abstract

Droughts are becoming more frequent and severe in Southwest China, with Yunnan being the most affected region. Most of the current studies on droughts in Yunnan are limited to individual cases and lack a common determination of the causes of historical drought events. In this study, we analyzed drought characteristics and causes over the last 60 years (1961-2020) in Yunnan Province in two seasons: dry and rainy. There was a clear trend of aridity in Yunnan Province in terms of both temporal and spatial changes, and there was a long-term drought period in approximately 2010; in particular, the frequency of drought in the dry season significantly increased. Due to its unique geographical location, precipitation in Yunnan Province is influenced by various factors, and the main influencing factors differed in different periods. SST variation is the most important factor affecting Yunnan drought, precipitation in Yunnan Province is affected by the warm pool of the Indian Ocean throughout the year, and thermal anomalies in different locations of the Pacific Ocean have different effects on Yunnan Province and often overlap with the effects of SST anomalies in the Indian Ocean.
云南省近 60 年(1961-2020 年)干旱特征及成因分析
中国西南地区的干旱日益频繁和严重,云南是受影响最严重的地区。目前对云南干旱的研究大多局限于个案,缺乏对历史干旱事件成因的共同判断。本研究分析了云南省近 60 年(1961-2020 年)旱、雨两季的干旱特征及成因。从时空变化来看,云南省干旱趋势明显,约在 2010 年出现了长期干旱,尤其是旱季干旱发生频率明显增加。由于其独特的地理位置,云南省降水受多种因素影响,不同时期的主要影响因素也不尽相同。SST 变化是影响云南干旱的最主要因素,云南省降水全年受印度洋暖池的影响,太平洋不同位置的热异常对云南省的影响不同,且往往与印度洋 SST 异常的影响重叠。
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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来源期刊
Journal of Hydrometeorology
Journal of Hydrometeorology 地学-气象与大气科学
CiteScore
7.40
自引率
5.30%
发文量
116
审稿时长
4-8 weeks
期刊介绍: The Journal of Hydrometeorology (JHM) (ISSN: 1525-755X; eISSN: 1525-7541) publishes research on modeling, observing, and forecasting processes related to fluxes and storage of water and energy, including interactions with the boundary layer and lower atmosphere, and processes related to precipitation, radiation, and other meteorological inputs.
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