East–West Reverse Coupling Between Spring Soil Moisture and Summer Precipitation and Its Possible Responsibility for Wet Bias in GCMs Over Tibetan Plateau-Reference-Cited by-同舟云学术

East–West Reverse Coupling Between Spring Soil Moisture and Summer Precipitation and Its Possible Responsibility for Wet Bias in GCMs Over Tibetan Plateau

Published:2022-04-05 Issue:7 Volume:127 Page:
ISSN:2169-897X
Container-title:Journal of Geophysical Research: Atmospheres
language:en
Short-container-title:JGR Atmospheres

Author:

Yang Kai¹^ORCID,Wang Chenghai¹^ORCID

Affiliation:

1. Key Laboratory of Arid Climate Resource and Environment of Gansu Province (ACRE) Research and Development Center of Earth System Model (RDCM) College of Atmospheric Sciences Lanzhou University Lanzhou China

Funder

National Natural Science Foundation of China

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2021JD036286

Reference74 articles.

1. Sensitivity of Precipitation Forecast Skill Scores to Bilinear Interpolation and a Simple Nearest-Neighbor Average Method on High-Resolution Verification Grids

2. Characteristics of GLDAS soil‐moisture data on the Tibet plateau;Bao H.;Sciences in Cold and Arid Regions,2017

3. Comparison of soil moisture in GLDAS model simulations and in situ observations over the Tibetan Plateau

4. MERRA‐2: Initial evaluation of the climate. NASA Technical report series on global modeling and data assimilation;Bosilovich M.;NASA/TM‐2015,2015

5. Evaluation of AMSR-E retrievals and GLDAS simulations against observations of a soil moisture network on the central Tibetan Plateau

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