Indian summer monsoon rainfall response to two distinct evolutions of La Niña events

IF 3.5 3区 地球科学 Q2 METEOROLOGY & ATMOSPHERIC SCIENCES International Journal of Climatology Pub Date : 2024-08-07 DOI:10.1002/joc.8588
Tanu Sharma, Satyaban B. Ratna, Damodara S. Pai, Arti Bandgar, Madhavan Rajeevan, Mrutyunjay Mohapatra, Onpathamkuniyil P. Sreejith, Krishnanand S. Hosalikar
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Abstract

This study examines the asymmetry in the Indian summer monsoon rainfall (ISMR) response over India and its four homogeneous regions to two distinct types of temporal evolution in La Niña. We have shown this uneven response by analysing the large-scale dynamics over tropical Indo-Pacific region for the period 1951–2022. We have identified two types of La Niña events during monsoon season (June–September) based on whether they evolved from El Niño or La Niña from preceding boreal winter season (December–February). India receives significantly more (less) rainfall during La Niña years, when it was preceded by El Niño (La Niña) in the preceding winter. We further observed the spatial diversity of rainfall over India with a northeast–southwest dipole pattern. When La Niña years were preceded by El Niño, positive surface pressure anomaly over west-north Pacific, low-level westerlies and moisture transport favoured the rainfall over south peninsula and west-central India. Whereas moisture divergence associated with anomalous lower-tropospheric anticyclone over west-north Pacific suppressed the rainfall over Indo-Gangetic plains. However, when La Niña years were preceded by La Niña in winter, the absence of westerlies and weak moisture transport subdued the rainfall over south peninsula and west-central India. At the same time, moisture convergence and a greater number of monsoon depressions favoured rainfall over north-west India. This study also looked at how well eight Copernicus Climate Change Service (C3S) models predicted ISMR and SST for two types of La Niña with April initial conditions during the period 1993–2016. Models were able to capture the spatial pattern of SST anomalies over Indo-Pacific Ocean, but all models could not capture the spatial pattern of ISMR. However, in terms of intensity, six out of eight models could predict more (less) ISMR when it was preceded by El Niño (La Niña), coinciding with the observed anomaly.

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印度夏季季风降雨对拉尼娜现象两种不同演变的响应
本研究探讨了印度及其四个同质地区的印度夏季季风降雨量(ISMR)对拉尼娜两种不同类型的时间演变的不对称响应。我们通过分析 1951-2022 年期间热带印度洋-太平洋地区的大尺度动态,显示了这种不均衡的响应。我们根据季风季节(6 月至 9 月)的拉尼娜现象是由厄尔尼诺现象演变而来,还是由之前寒带冬季(12 月至 2 月)的拉尼娜现象演变而来,确定了季风季节(6 月至 9 月)的两种拉尼娜现象。如果在拉尼娜现象发生之前的冬季出现过厄尔尼诺现象(拉尼娜现象),则印度在拉尼娜现象发生年份的降雨量会明显增加(减少)。我们进一步观察到印度降雨的空间多样性,呈现东北-西南偶极模式。当拉尼娜年之前出现厄尔尼诺现象时,西北太平洋西部的正表面气压异常、低层西风和水汽输送有利于印度半岛南部和中西部的降雨。而与北太平洋西部低对流层反气旋异常相关的水汽辐散则抑制了印度-甘肃平原的降雨。然而,当拉尼娜年之前的冬季出现拉尼娜现象时,西风的缺失和水汽输送的减弱抑制了印度半岛南部和中西部的降雨。同时,水汽辐合和更多的季风凹陷有利于印度西北部的降雨。这项研究还考察了哥白尼气候变化服务(C3S)的八个模型在 1993-2016 年期间对两种类型的拉尼娜(初始条件为四月)的 ISMR 和 SST 的预测效果。模型能够捕捉印度洋-太平洋海温异常的空间模式,但所有模型都无法捕捉 ISMR 的空间模式。然而,就强度而言,当厄尔尼诺现象(拉尼娜现象)出现之前,8 个模式中有 6 个模式可以预测较多(较少)的 ISMR,这与观测到的异常相吻合。
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来源期刊
International Journal of Climatology
International Journal of Climatology 地学-气象与大气科学
CiteScore
7.50
自引率
7.70%
发文量
417
审稿时长
4 months
期刊介绍: The International Journal of Climatology aims to span the well established but rapidly growing field of climatology, through the publication of research papers, short communications, major reviews of progress and reviews of new books and reports in the area of climate science. The Journal’s main role is to stimulate and report research in climatology, from the expansive fields of the atmospheric, biophysical, engineering and social sciences. Coverage includes: Climate system science; Local to global scale climate observations and modelling; Seasonal to interannual climate prediction; Climatic variability and climate change; Synoptic, dynamic and urban climatology, hydroclimatology, human bioclimatology, ecoclimatology, dendroclimatology, palaeoclimatology, marine climatology and atmosphere-ocean interactions; Application of climatological knowledge to environmental assessment and management and economic production; Climate and society interactions
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