Cloud Radiative Feedback to the Large‐Scale Atmospheric Circulation Greatly Reduces Monsoon‐Season Wet Bias Over the Tibetan Plateau in Climate Modeling

Cloud Radiative Feedback to the Large‐Scale Atmospheric Circulation Greatly Reduces Monsoon‐Season Wet Bias Over the Tibetan Plateau in Climate Modeling

Abstract Over‐estimation of summer precipitation over the Tibetan Plateau (TP) is a well‐known and persistent problem in most climate models. This study demonstrates the impact of a Gaussian Probability Density Function cloud fraction scheme on rainfall simulations using the Weather Research and For...

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Bibliographic Details
Main Authors: Jiarui Liu, Kun Yang, Dingchi Zhao, Peili Wu, Jiamin Wang, Xu Zhou, Yanluan Lin, Hui Lu, Yaozhi Jiang, Jiancheng Shi
Format: Article
Language:English
Published: Wiley 2024-07-01
Series:Geophysical Research Letters
Subjects:
cloud radiative feedback
large‐scale atmospheric circulation
wet bias
Tibetan Plateau
cloud fraction scheme
climate modeling
Online Access:https://doi.org/10.1029/2024GL109180
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https://doi.org/10.1029/2024GL109180

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