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Indian Ocean warming modulates Pacific climate change
Author(s) -
JingJia Luo,
Wataru Sasaki,
Yukio Masumoto
Publication year - 2012
Publication title -
proceedings of the national academy of sciences
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 5.011
H-Index - 771
eISSN - 1091-6490
pISSN - 0027-8424
DOI - 10.1073/pnas.1210239109
Subject(s) - climatology , climate change , radiative forcing , oceanography , abrupt climate change , centennial , pacific decadal oscillation , environmental science , climate model , effects of global warming on oceans , global warming , atmosphere (unit) , walker circulation , pacific ocean , ocean heat content , effects of global warming , geography , ocean current , sea surface temperature , geology , meteorology , archaeology
It has been widely believed that the tropical Pacific trade winds weakened in the last century and would further decrease under a warmer climate in the 21st century. Recent high-quality observations, however, suggest that the tropical Pacific winds have actually strengthened in the past two decades. Precise causes of the recent Pacific climate shift are uncertain. Here we explore how the enhanced tropical Indian Ocean warming in recent decades favors stronger trade winds in the western Pacific via the atmosphere and hence is likely to have contributed to the La Niña-like state (with enhanced east-west Walker circulation) through the Pacific ocean-atmosphere interactions. Further analysis, based on 163 climate model simulations with centennial historical and projected external radiative forcing, suggests that the Indian Ocean warming relative to the Pacific's could play an important role in modulating the Pacific climate changes in the 20th and 21st centuries.

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