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    Diversity of MJO Initiation Regions and Processes 

    Source: Journal of Climate:;2022:;volume( 035 ):;issue: 020:;page 3121
    Author(s): Tianyi Wang; Tim Li
    Publisher: American Meteorological Society
    Abstract: The diversity of the Madden–Julian oscillation (MJO) initiation (i.e., initial onset of active convection before moving eastward) regions was explored using a clustering method. Regions favorable for MJO initiations are ...
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    Asymmetric Impacts of El Niño and La Niña on Equatorial Atlantic Warming 

    Source: Journal of Climate:;2022:;volume( 036 ):;issue: 001:;page 193
    Author(s): Leishan Jiang; Tim Li; Yoo-Geun Ham
    Publisher: American Meteorological Society
    Abstract: Despite an insignificant linear relation between the boreal summer equatorial Atlantic sea surface temperature anomaly (EA SSTA) and preceding winter El Niño–Southern Oscillation (ENSO), an EA warming event was found to ...
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    Role of a Pacific Easterly Wave in the Genesis of Hagupit (2008) 

    Source: Weather and Forecasting:;2022:;volume( 037 ):;issue: 012:;page 2183
    Author(s): Chen Zhao; Tim Li; Mingyu Bi
    Publisher: American Meteorological Society
    Abstract: The Advanced version of the Weather Research and Forecasting (WRF-ARW) Model is used to investigate the influence of an easterly wave (EW) on the genesis of Typhoon Hagupit (2008) in the western North Pacific. Observational ...
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    Impacts of CP and EP El Niño Events on the Antarctic Sea Ice in Austral Spring 

    Source: Journal of Climate:;2021:;volume( 034 ):;issue: 023:;page 9327
    Author(s): Zhang, Chao;Li, Tim;Li, Shuanglin
    Publisher: American Meteorological Society
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    Distinctive Rainfall Evolutions in East Asia between Super and Regular El Niño Events during Their Decaying Summers 

    Source: Journal of Climate:;2022:;volume( 036 ):;issue: 001:;page 155
    Author(s): Xiaohui Wang; Tim Li; Suxiang Yao
    Publisher: American Meteorological Society
    Abstract: While enhanced rainbands progressed northward in East Asia from June to August during the regular El Niño decaying summer, strengthened rainbands were only observed in the earlier summer and disappeared in August in the ...
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