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Sensitivity of simulated tropical intraseasonal oscillations to cumulus schemes

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Abstract

The sensitivity of simulated tropical intraseasonal oscillations (ISO) to different cumulus parameterization schemes was analyzed using an atmospheric general circulation model (latest version-SAMIL2.2.3) developed at the Laboratory for Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics (LASG) at the Institute of Atmospheric Physics (IAP) of the Chinese Academy of Sciences. Results show that the basic features of tropical climatological intraseasonal oscillations (CISO) can be captured using all three cumulus schemes. The CISO simulated by the Tiedtke scheme was found to be more realistic than that of the Manabe and Zhang-McFarlane schemes. The results of simulated transient intraseasonal oscillations (TISO) indicate that although the Tiedtke and the Zhang-McFarlane schemes in the new version SAMIL2.2.3 have been adjusted according to different problems, only the latter can simulate the eastward propagation of the 27–50-day TISO mode. It may be associated with the more realistic diabatic heating profile simulated by the Zhang-McFarlane scheme. In addition, the Manabe scheme in SAMIL2.2.3 is the same as that in the prior version SAMIL2.08. However, some aspects of the physical process, such as the radiation scheme and aerosol condition, have been changed. Conversely the eastward propagation from 100°E to the west of the tropical 27–50-day TISO mode only can be simulated using the Manabe scheme of SAMIL 2.08. Consequently, not all the improvements of physical parameterization schemes work well in every respect. The coordinated developments between dynamic frame and physical processes, and among different physical processes, are important methods that may be used to improve the model.

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Correspondence to AnMin Duan.

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Hu, W., Duan, A. & Wu, G. Sensitivity of simulated tropical intraseasonal oscillations to cumulus schemes. Sci. China Earth Sci. 54, 1761–1771 (2011). https://doi.org/10.1007/s11430-011-4215-0

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