Regionality of long-term trends and interannual variation of seasonal precipitation over India

被引：34

作者：

Fukushima, Azusa ^{[1
]}

Kanamori, Hironari ^{[2
]}

Matsumoto, Jun ^{[3
,4
]}

机构：

[1] Kobe Gakuin Univ, Fac Humanities & Sci, Nishi Ku, 518 Arise,Ikawadani Cho, Kobe, Hyogo 6512180, Japan

[2] Nagoya Univ, Inst Space Earth Environm Res, Chikusa Ku, Furo Cho, Nagoya, Aichi 4648601, Japan

[3] Tokyo Metropolitan Univ, Dept Geog, Res Ctr Climatol, 1-1 Minamiosawa, Hachioji, Tokyo 1920397, Japan

[4] Japan Agcy Marine Earth Sci & Technol, Dept Coupled Ocean Atmosphere Land Proc Res, 2-15 Natsushima Cho, Yokosuka, Kanagawa 2370061, Japan

来源：

PROGRESS IN EARTH AND PLANETARY SCIENCE | 2019年 / 6卷 / 1期

关键词：

Indian monsoon variability; Rainfall seasonality; Cluster analysis; Water vapor convergence; Low-level jet stream; NORTHEAST MONSOON RAINFALL; SOUTHWEST MONSOON; INCREASING TREND; VARIABILITY; OCEAN; ZONES; BREAK;

D O I：

10.1186/s40645-019-0255-4

中图分类号：

P [天文学、地球科学];

学科分类号：

07 ;

摘要：

This study investigated the long-term trends and interannual variations (IAVs) of seasonal precipitation during two different periods in India and their relation to atmospheric circulation. To focus on the relation between the regional characteristics of precipitation and the large-scale circulation system, we defined homogeneous regions based on pentad rainfall seasonality using hierarchical cluster analysis. Seven obtained clusters (regions) were used to analyze the long-term trends, IAVs, and their relation to atmospheric circulation. Seasonal precipitation showed no remarkable trend in most regions and seasons, which implies the effect of IAV in seasonal precipitation is greater than the long-term trend. Based on regression analysis, the IAV of seasonal precipitation and its relation to atmospheric circulation over the ocean surrounding India were detected for each season. Enhancement of the southwesterly monsoon flow over the Indian Ocean and the strength of the southeasterly wind related to the activity of the monsoon trough around the Gangetic Plain both affected the increase of summer monsoon precipitation in regions CL3 (central and eastern India) and CL6 (western coast of the Arabian Sea in southern India). In contrast, neither region CL5 (eastern coastal region of southern India) nor CL7 (northeastern India and part of the western coastal region of southern India) showed a relationship between IAV of summer monsoon precipitation and the southwesterly flow or the southeasterly flow over the Indian Ocean or the Gangetic Plain, respectively. Region CL5 showed strong correlation with the northeasterly monsoon flow (strength of the southeasterly flow over the Bay of Bengal) during the post-monsoon season. Other regions showed no relation with the northeasterly flow during the post-monsoon season. Furthermore, IAV of precipitation in region CL7 showed no correlation with either the southwesterly monsoon during the summer monsoon season or the northeasterly monsoon during the post-monsoon season.

引用

页数：20

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