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

Bibliographic Details
Main Authors: Helin Wei, David H. Bromwich, Ying-hwa Kuo, Tae Kwon Wee
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
Antarctic
The Antarctic
Antarc*
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.590.7500
Description
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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