Understanding of CMIP6 surface temperature cold bias over the westerly and monsoon regions of the Tibetan Plateau
Author:
Funder
Key Technologies Research and Development Program
Shanghai Municipal Education Commission
China Scholarship Council
Publisher
Springer Science and Business Media LLC
Link
https://link.springer.com/content/pdf/10.1007/s00382-024-07122-4.pdf
Reference90 articles.
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2. Bansod SD, Fadnavis S, Ghanekar SP (2015) Association of the pre-monsoon thermal field over north India and the western Tibetan Plateau with summer monsoon rainfall over India. Ann. Geophys. 33(8):1051–1058. https://doi.org/10.5194/angeo-33-1051-2015
3. Bao Y, You Q (2019) How do westerly jet streams regulate the winter snow depth over the Tibetan Plateau? Climate Dynam 53(1):353–370. https://doi.org/10.1007/s00382-018-4589-1
4. Beltrami H, Kellman L (2003) An examination of short- and long-term air–ground temperature coupling. Glob Planet Change 38(3):291–303. https://doi.org/10.1016/S0921-8181(03)00112-7
5. Cai Z, You Q, Chen HW et al (2022) Amplified wintertime Barents Sea warming linked to intensified Barents oscillation. Environ Res Lett 17(4):044068. https://doi.org/10.1088/1748-9326/ac5bb3
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