File:Circulation Northeaster.png

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Description Typical upper level circulation for a Nor'easter Storm. The trough along the Appalachian brings cold air to the East Coast where it meets the Gulf Stream. Patrons typique de la circulation d'altitude pour le développement d'une Tempête du cap Hatteras: le creux barométrique amène de l'air arctique au-dessus du Gulf Stream.
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Source NOAA
Author Pierre cb
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This image is in the public domain because it contains materials that originally came from the U.S. National Oceanic and Atmospheric Administration, taken or made as part of an employee's official duties.

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Date/TimeThumbnailDimensionsUserComment
current20:00, 19 March 2007Thumbnail for version as of 20:00, 19 March 2007522 × 644 (44 KB)Pierre cb (talk | contribs){{Information |Description= Typical upper level circulation for a Nor'easter Storm. The trough along the Appalachian brings cold air to the East Coast where it meets the Gulf Stream. Patrons typique de la circulation d'altitude pour le développement d'un

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