Abstract

This chapter discusses the general aspects of deducing a consistent cloud parameterization scheme, designed to predict fractional cloud cover and precipitation amounts and distribution in large-scale models. For specific background conditions, such as the supply of cloud condensation nuclei and large-scale and mesoscale circulations, the development of hydrometeors is governed by cloud microphysical processes. Cloud cover is determined by humidity and air motions, resulting from both the larger-scale background circulation and the release of latent heat on smaller scales. Owing to nonlinearities, the parameterizations of these two widely separated scale regimes are not completely decoupled. The chapter presents general formulations for the parameterizations of clouds in large-scale models. It is the value, or functional form, of the obtained parameters that account for different types or situations of condensation–cloud processes. Such differentiation is discussed with regard to both microphysical and subgrid-scale aspects. The chapter reveals that measurements provides the valuable data needed for testing algorithms used to relate measured radiances to cloud parameters.

Full Text
Paper version not known

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call

Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.