5B.6 A CASE STUDY OF POLAR MM5 USAGE FOR MESOSCALE NUMERICAL WEATHER PREDICTION IN THE ANTARCTIC: UPPER BOUNDARY CONDITION
1 In limited area modeling, the upper boundary condition was not addressed extensively until nonhydrostatic models became widely available for numerical weather prediction (Mesinger, 1997). Ideally
Main Authors: | , , , |
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Language: | English |
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Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.590.7500 |
Summary: | 1 In limited area modeling, the upper boundary condition was not addressed extensively until nonhydrostatic models became widely available for numerical weather prediction (Mesinger, 1997). Ideally |
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