1 / 32

WINTER STORMS

WINTER STORMS. MSC 118, 2/12/14. Prof. Sharan Majumdar. http://orca.rsmas.miami.edu/~majumdar. Outline. 1 . Structure and Formation of Winter Storms 2. Winter Weather in Jan-Feb 2014 Polar Vortex Alberta Clipper Atlanta two weeks ago Today’s storm!. 1. Structure of Winter Storms.

mandar
Télécharger la présentation

WINTER STORMS

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript

  1. WINTER STORMS MSC 118, 2/12/14. Prof. Sharan Majumdar. http://orca.rsmas.miami.edu/~majumdar

  2. Outline 1. Structure and Formation of Winter Storms 2. Winter Weather in Jan-Feb 2014 • Polar Vortex • Alberta Clipper • Atlanta two weeks ago • Today’s storm!

  3. 1. Structure of Winter Storms Typical structure of most winter storms, although they can be very different.

  4. A Typical Winter Storm Surface low pressure system, usually <1000 mb. Warm and cold fronts, although the low may be occluded (fronts weakened). Heaviest rain or snow in the ‘head’ of the storm system, with possible banding. Squally rain or snow along the cold front.

  5. Winter storm formation: Ingredients Favorable jet stream position aloft. Cold polar air coming from north. Sharp ‘temperature gradient’. Availability of moisture.

  6. Norwegian Cyclone Model • Initial ‘frontal boundary’ separating cold and warm air. • A “wave” forms along the front as an upper-air disturbance in the jet stream moves over it. • Front develops a kink where wave develops.

  7. Isobars Isotherms

  8. 2a. Polar Vortex: January 2014

  9. “The planetary-scale cyclonic circulation, centered generally in the polar regions, extending from the middle troposphere to thestratosphere. The westerly airflow is largely a manifestation of the thermal wind above the polar frontal zone of middle and subpolar latitudes. The vortex is strongest in winter when the pole-to-equator temperature gradient is strongest. In the Northern Hemisphere, the vortex has two centers in the mean, one near Baffin Island and the other over northeast Siberia”. AMS Glossary of Meteorology

  10. Winds in the stratosphere

  11. Winds in the stratosphere

  12. 2b. Alberta Clipper Storms, Jan-Feb 2014 “A fast moving low pressure system that moves southeast out of Canadian Province of Alberta (southwest Canada) through the Plains, Midwest, and Great Lakes region usually during the winter. This low pressure area is usually accompanied by light snow, strong winds, and colder temperatures.” AMS Glossary of Meteorology

  13. Craziness in Atlanta, 1/28/14 National Weather Service Summary

  14. This week’s storm (11-13 Feb 2014)

  15. Will this NAM forecast verify?

  16. Nor’Easter • A cyclonic storm of the east coast of North America, so called because the winds over the coastal area are from the northeast. • They may occur at any time of year but are most frequent and most violent between September and April. Northeast storms usually develop in lower–middle latitudes (30°–40°N) within 100 miles east or west of the coastline. They progress generally northward to northeastward and typically attain maximum intensity near New England and the Maritime Provinces. AMS Glossary of Meteorology

More Related