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• W2112304371 abstract "As faster computers emerge, resolution continues to improve in weather-prediction and climate models. How does this affect the problems that we are dealing with in the models? In this study we have concentrated on one of these problems, namely the treatment of clouds. Among the questions addressed are: How do cloud-related processes (condensation, precipitation) depend on grid resolution? How should we take this into account? Can we simulate orographic clouds when we have a grid resolution of hundreds of kilometres (climate models)? To tackle these questions simulations are performed with a limited-area model that is run with horizontal grid resolutions of 150,50 and 25 km. The model has a sophisticated treatment of condensation and clouds. For verification, use is made of satellite-derived cloud water content and cloud cover, and surface observations of precipitation.It is found that when resolution is enhanced, precipitation systematically increases while cloud cover decreases. The main reason is that much stronger vertical motions develop at high resolution, yielding dense, narrow clouds, with clear air between. The consequences of these results for cloud parametrization are discussed. It is further shown that cloud-cover simulations over mountainous terrain can be improved by paying regard to the sub-grid-scale orography." @default.
• W2112304371 created "2016-06-24" @default.
• W2112304371 creator A5071309631 @default.
• W2112304371 date "1991-10-01" @default.
• W2112304371 modified "2023-10-04" @default.
• W2112304371 title "Cloud parametrization at different horizontal resolutions" @default.
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• W2112304371 doi "https://doi.org/10.1002/qj.49711750207" @default.
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