South Asian summer rainfall from CMIP3 to CMIP6 models: biases and improvements
Author:
Funder
National Natural Science Foundation of China
Publisher
Springer Science and Business Media LLC
Subject
Atmospheric Science
Link
https://link.springer.com/content/pdf/10.1007/s00382-022-06542-4.pdf
Reference49 articles.
1. Acosta RP, Huber M (2017) The neglected Indo-Gangetic Plains low-level jet and its importance for moisture transport and precipitation during the peak summer monsoon. Geophys Res Lett 44:8601–8610. https://doi.org/10.1002/2017GL074440
2. Annamalai H, Taguchi B, McCreary JP et al (2017) Systematic errors in South Asian monsoon simulation: importance of equatorial Indian Ocean processes. J Clim 30:8159–8178. https://doi.org/10.1175/JCLI-D-16-0573.1
3. Annamalai H, Boos WR, Martin G et al (2021) Grand challenges in asian summer monsoon modeling - representation of processes and sources of model error. In: The Multiscale Global Monsoon System. 367–386
4. Bollasina M, Nigam S (2009) Indian Ocean SST, evaporation, and precipitation during the South Asian summer monsoon in IPCC-AR4 coupled simulations. Clim Dyn 33:1017–1032. https://doi.org/10.1007/S00382-008-0477-4/FIGURES/10
5. Boos WR, Hurley JV (2013) Thermodynamic bias in the multimodel mean boreal summer monsoon. J Clim 26:2279–2287. https://doi.org/10.1175/JCLI-D-12-00493.1
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