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The top documents tagged [warm air advection]
FLURRIES OR FEET? An Analysis of QPF Errors in an Eastern North Carolina Snowstorm December 2-4, 2000 Jason Caldwell South Carolina State Climate Office
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In diagnosing tropical cyclone cyclogenesis and intensification we are interested in the 850 to 500hPa wind profiles. We have observed the heaviest rainfall
217 views
Mesoscale Banded Precipitation EAX Winter Weather Workshop 28 October 2008 EAX Winter Weather Workshop 28 October 2008
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Boundary Layer Clouds & Sea Spray Steve Siems, Yi (Vivian) Huang, Luke Hande, Mike Manton & Thom Chubb
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Echo Tops Fairly accurate at depicting height of storm tops Inaccurate data close to radar because there is no beam angle high enough to see tops. Often
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Atms 4320 / 7320 – Lab 7 The Thermal Wind: Forecasting Problems and the Analysis of Fronts
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Cold Air Damming
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Formation of the Extratropical Cyclone (Cyclogenesis)
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Formation of the Extratropical Cyclone (Cyclogenesis)
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Formation of the Extratropical Cyclone (Cyclogenesis)
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