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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https://doi.org/10.1007/978-3-662-61740-3ipitation annual cycle accurately. Here, we review and examine the nature and dynamical causes of their biases. We discuss the coupled nature of the monsoon annual cycle from observations and then present errors in multi-model-mean, climatological fields of ocean–atmosphere variables determined from

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https://doi.org/10.1007/978-3-662-61766-3is our benchmark. These challenges comprise four main areas of developments: making optimal use of the available observational data to obtain the best analysis, advanced ensemble methods to predict the uncertainties in the analyses and forecasts, model developments to better represent shallow and de

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Petrus Apianus und der Dreisatzf parameterizing convection based on parcel theory. Formulated to take into account the role of atmospheric mixing within the boundary layer, the HCF uses profiles of temperature and humidity to quantify how conditioned the atmosphere is to moist free convection. The initiation of convection is eval

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Wie kommt man auf Quaternionen?n of Indian summer monsoon. The location of maximum precipitation and CAPE does not always coincide in a CRM simulation. The diurnal land surface heating is shown to have an effect on CAPE and precipitation over ocean. Convective inhibition energy is shown to have a significant effect on the locatio

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https://doi.org/10.1007/978-3-662-62562-0ast System version 2 (CFSV2). The resulting model is referred to here as CFSsmcm. Two 15-year-long climate simulations of the CFSsmcm, differing only by one SMCM parameter, namely, the mid-tropospheric dryness parameter, MTD0 are analyzed and interpreted here. This particular parameter is chosen bec

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Regina Toepfer,Peter Burschel,Jörg Weschenstitute of Tropical Meteorology, in order to address key questions pertaining to the science of Climate Change. The IITM-ESM has been developed by transforming a state-of-the-art seasonal prediction model into a radiatively balanced climate modeling framework suitable for investigating long-term cl

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