Titlebook: Current Trends in the Representation of Physical Processes in Weather and Climate Models; David A. Randall,J. Srinivasan, Parthasarathi Mu

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Convection Initiation in Climate Models Using the Heated Condensation Framework: A Review,ate perspective, applying the HCF trigger to the Community Earth System Model reduces convective overactivity in the model and improves the frequency of intense precipitation events. The use of the HCF as a convective trigger is still under active investigation, and strategies for including the effe

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Convective Available Potential Energy and Precipitation in a Cloud-Resolving Model Simulation of Innot include any representation of organized mesoscale convective systems. We show that CAPE consumed by these systems not only triggers vertical motion but also contributes to horizontal motion of the system.

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A Gray Zone GCM with Full Representation of Cloud Microphysics,equencies and the MJO reasonably well, although the MJO intensity is rather strong. Both cloud microphysics and scale-dependent deep convection play important roles in simulating a realistic MJO in the present GCM. Also noted is that the precipitation climatologies of the present atmospheric GCM (AG

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Cumulus Friction in the Asian Monsoon of a Global Model with 7 km Mesh,ection and shear are both strong, the viscosity can be characterized by a regression coefficient with values of about 5% cm., meaning that convection which yields 1 cm of precipitation decrements SKE by about 5%. Adjustment of balanced monsoon flow to such a viscous effect implies adiabatic ascent t

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