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Wei-Ting Chen, Chien-Ming Wu, and Hsi-Yen Ma

noted that Sperber et al. (2013) evaluated the Asian monsoon performance in CMIP3 and CMIP5 models using these metrics, and the CCSM4 (the coupled version of CAM4) is actually one of the top-performing models. Here we are trying to identify specific regions where obvious biases still exist in CAM5 AMIP. Over the oceanic regions where the monsoon domain is missing or the monsoon intensity is underestimated (over the BoB, EA, SCS, and WNP), the CAM5 AMIP shows earlier onset by four pentads or more

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Emily M. Riley Dellaripa, Eric D. Maloney, Benjamin A. Toms, Stephen M. Saleeby, and Susan C. van den Heever

. Acad. Sci. USA , 107 , 11 217 – 11 222 , https://doi.org/10.1073/pnas.0910818107 . 10.1073/pnas.0910818107 Emanuel , K. A. , and M. Živković-Rothman , 1999 : Development and evaluation of a convection scheme for use in climate models . J. Atmos. Sci. , 56 , 1766 – 1782 , https://doi.org/10.1175/1520-0469(1999)056<1766:DAEOAC>2.0.CO;2 . 10.1175/1520-0469(1999)056<1766:DAEOAC>2.0.CO;2 Hagos , S. M. , C. Zhang , Z. Feng , C. D. Burleyson , C. De Mott , B. Kerns , J. J

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Kyle Chudler, Weixin Xu, and Steven A. Rutledge

Fig. 9 . The red star in (b) is the launch location of the atmospheric soundings discussed in section 2d . These offshore rainfall maxima have previously been examined in modeling studies. Ogura and Yoshizaki (1988) utilized a two-dimensional cloud model to examine the Western Ghats precipitation maximum. They found that both vertical wind shear and ocean surface fluxes contributed to the offshore precipitation maximum. When either of these factors were suppressed in the model simulations, the

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