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Interannual variability of boreal summer intraseasonal oscillation over the northwestern Pacific influenced by the Pacific Meridional Mode

作     者:Haoyu Zhou Pang-Chi Hsu Lin Chen Yitian Qian Haoyu Zhou;Pang-Chi Hsu;Lin Chen;Yitian Qian

作者机构:Key Laboratory of Meteorological DisasterMinistry of Education/Joint International Research Laboratory of Climate and Environmental Change/Collaborative Innovation Center on Forecast and Evaluation of Meteorological DisastersNanjing University of Information Science and TechnologyNanjingChina 

出 版 物:《Atmospheric and Oceanic Science Letters》 (大气和海洋科学快报(英文版))

年 卷 期:2025年第18卷第1期

页      面:6-11页

核心收录:

学科分类:07[理学] 0707[理学-海洋科学] 

基  金:supported by the National Natural Science Foundation of China [grant number 42088101] 

主  题:Boreal summer intraseasonal oscillation Interannual variability Pacific Meridional Mode Moisture budget analysis 

摘      要:During the boreal summer,intraseasonal oscillations exhibit significant interannual variations in intensity over two key regions:the central-western equatorial Pacific(5°S-5°N,150°E-150°W)and the subtropical Northwestern Pacific(10°-20°N,130°E-175°W).The former is well-documented and considered to be influenced by the ENSO,while the latter has received comparatively less attention and is likely influenced by the Pacific Meridional Mode(PMM),as suggested by partial correlation analysis *** elucidate the physical processes responsible for the enhanced(weakened)intraseasonal convection over the subtropical northwestern Pacific during warm(cold)PMM years,the authors employed a moisture budget *** findings reveal that during warm PMM years,there is an increase in summer-mean moisture over the subtropical northwestern *** increase interacts with intensified vertical motion perturbations in the region,leading to greater vertical moisture advection in the lower troposphere and consequently resulting in convective *** a process is pivotal in amplifying intraseasonal convection *** observational findings were further verified by model experiments forced by PMM-like sea surface temperature patterns.

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