Slide 1FLURRIES OR FEET? An Analysis of QPF Errors in an Eastern North Carolina Snowstorm December 2-4, 2000 Jason Caldwell South Carolina State Climate Office Slide 2 WINTER…

Slide 1In diagnosing tropical cyclone cyclogenesis and intensification we are interested in the 850 to 500hPa wind profiles. We have observed the heaviest rainfall all over…

Slide 1Mesoscale Banded Precipitation EAX Winter Weather Workshop 28 October 2008 EAX Winter Weather Workshop 28 October 2008 Slide 2 Norwegian Cycle Model Slide 3 Relatively…

Slide 1Boundary Layer Clouds & Sea Spray Steve Siems, Yi (Vivian) Huang, Luke Hande, Mike Manton & Thom Chubb Slide 2 Slide 3 (Huang et al. 2012) CloudSat climatology…

Slide 1 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 has stair-stepped…

Slide 1 Atms 4320 / 7320 – Lab 7 The Thermal Wind: Forecasting Problems and the Analysis of Fronts Slide 2 Thermal wind: Bluestein p 181 - 187, and Holton p 68 - 71. The…

Cold Air Damming Cold Air Damming What is Cold Air Damming? Cold Air Damming Cold Air Damming is when cold air is locked or “dammed” into a location, often a valley or…

Slide 1 Formation of the Extratropical Cyclone (Cyclogenesis) geog-www.sbs.ohio-state.edu/courses/G620/.../ASP620Lecture10.ppt Cyclogenesis Extratropical cyclones often form…

Slide 1 Formation of the Extratropical Cyclone (Cyclogenesis) geog-www.sbs.ohio-state.edu/courses/G620/.../ASP620Lecture10.ppt Cyclogenesis Extratropical cyclones often form…

Formation of the Extratropical Cyclone (Cyclogenesis) Cyclogenesis Extratropical cyclones often form when an upper level trough (e.g. a shortwave) approaches a front that…