WEATHER TERMINOLOGY



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J

JET STREAM
An area of strong winds that are concentrated in a relatively narrow band in the upper troposphere of the middle latitudes and subtropical regions of the Northern and Southern Hemispheres. Flowing in a semi-continuous band around the globe from west to east, it is caused by the changes in air temperature where the cold polar air moving towards the equator meets the warmer equatorial air moving polarward. It is marked by a concentration of isotherms and strong vertical shear. Various types include the arctic, the low level, the polar, and the subtropical jets.

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SOURCES

Branick, Michael. NOAA Technical Memorandum NWS SR-145, A Comprehensive Glossary of Weather Terms for Storm Spotters. U.S. Department of Commerce, 1995.

Everything Weather - The Essential Guide to the Whys and Wonders of Weather.

Famighetti, Robert (ed.). The World Almanac and Book of Facts (1996). Mahwah, New Jersey. Funk & Wagnalls Corporation, 1995.

Federal Meteorological Handbook No. 1, Surface Weather Observations and Reports. National Weather Service, U.S. Department of Commerce, 1996.

Huschke, R.E. (ed.). The Glossary of Meteorology. Boston, Massachusetts. American Meteorological Society Press, 1980.

National Weather Service Observing Handbook No. 7, Surface Weather Observations and Reports. U.S. Department of Commerce, 1996.