Interdecadal Shifts in the Winter Monsoon Rainfall of the Philippines

被引:11
|
作者
Olaguera, Lyndon Mark [1 ]
Matsumoto, Jun [1 ,2 ]
Kubota, Hisayuki [2 ,3 ]
Inoue, Tomoshige [1 ]
Cayanan, Esperanza O. [4 ]
Hilario, Flaviana D. [4 ]
机构
[1] Tokyo Metropolitan Univ, Dept Geog, 1-1 Minami Osawa, Hachioji, Tokyo 1920397, Japan
[2] Japan Agcy Marine Earth Sci & Technol, Dept Coupled Ocean Atmosphere Land Proc Res, Yokosuka, Kanagawa 2370061, Japan
[3] Hokkaido Univ, Dept Earth & Planetary Sci, Fac Sci, Kita Ku, Kita 10,Nishi 8, Sapporo, Hokkaido 0600810, Japan
[4] Philippine Atmospher Geophys & Astron Serv Adm, Quezon City 1100, Philippines
来源
ATMOSPHERE | 2018年 / 9卷 / 12期
基金
日本学术振兴会; 日本科学技术振兴机构;
关键词
Philippines; subseasonal variability; interdecadal variability; tropical cyclones; winter monsoon; Pacific Decadal Oscillation (PDO); PACIFIC ANOMALOUS ANTICYCLONE; TROPICAL CYCLONE ACTIVITY; SEA-SURFACE TEMPERATURE; SOUTH CHINA SEA; SUMMER MONSOON; SEASONAL MARCH; PART II; THERMODYNAMIC PROCESSES; MARITIME CONTINENT; CLIMATE CHANGES;
D O I
10.3390/atmos9120464
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
This study investigates the interdecadal shifts in the winter monsoon (November to March) rainfall of the Philippines from 1961 to 2008. Monthly analysis of the winter monsoon rainfall shows that the shifts are most remarkable during December. In particular, two interdecadal shifts are identified in the December rainfall time series around 1976/1977 and 1992/1993. To facilitate the examination of the possible mechanisms leading to these shifts, the analysis period is divided into three epochs: 1961-1976 (E1), 1977-1992 (E2), and 1993-2008 (E3). The mean and interannual variability of rainfall during E2 are suppressed compared with the two adjoining epochs. The shift around 1976/1977 is related to the phase shift of the Pacific Decadal Oscillation (PDO) from a negative phase to a positive phase and features an El Nino-like sea surface temperature (SST) change over the Pacific basin, while that around 1992/1993 is related to a La Nina-like SST change. Further analysis of the largescale circulation features shows that the decrease in the mean rainfall during E2 can be attributed to the weakening of the low-level easterly winds, decrease in moisture transport, and decrease in tropical cyclone activity. In addition, the suppressed interannual variability of rainfall during E2 can be partly attributed to the El Nino-like SST change and the weakening of the East Asian winter monsoon.
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页数:25
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