Influence of SST-precipitation relationship over the equatorial western Pacific on simulation of the Madden-Julian Oscillation
ID:1173 View Protection:ATTENDEE Updated Time:2024-10-14 10:41:48 Hits:733 Oral (invited)

Start Time:2025-01-14 10:25(Asia/Shanghai)

Duration:15min

Session:S65 Session 65-Oceanic-Atmospheric Processes Over the Indian and Western Pacific Oceans » S65-1Oceanic-Atmospheric Processes over the Indian and Western Pacific Oceans

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Abstract
Capabilities of 43 models of the Coupled Model Intercomparison Project Phase 6 (CMIP6) to simulate the Madden-Julian Oscillation (MJO) were compared in this study. Models with higher MJO simulation skills reproduce organized large-scale convection more frequently over the equatorial western Pacific (EWP), suggesting that MJO simulations are tightly connected to organization of large-scale precipitation over the EWP. MJO simulation skills are not significantly correlated with the mean sea surface temperature (SST) over the EWP, but tightly connected to SST threshold for convection there. The top simulations exhibit lower SST threshold and more realistic SST-precipitation relationship over the EWP, suggesting that convection can be organized more easily and intensified more rapidly with the increasing SST in these simulations. Our results emphasize that reproducing the relationship between SST and large-scale precipitation over the EWP is critical to MJO simulations. 
Keywords
Madden-Julian Oscillation,sea surface temperature,Precipitation,western Pacific
Speaker
Jian Ling
Professor Institute of Atmospheric Physics, Chinese Academy of Sciences

Submission Author
Jian Ling Institute of Atmospheric Physics, Chinese Academy of Sciences
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Important Date
  • Conference Date

    Jan 13

    2025

    to

    Jan 17

    2025

  • Sep 27 2024

    Draft paper submission deadline

  • Feb 17 2025

    Registration deadline

Sponsored By
State Key Laboratory of Marine Environmental Science, Xiamen University
Organized By
State Key Laboratory of Marine Environmental Science, Xiamen University
Department of Earth Sciences, National Natural Science Foundation of China
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