File:Bande brillante Brightband fr.png

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Bande_brillante_Brightband_fr.png ‎(383 × 501 pixels, file size: 11 KB, MIME type: image/png)

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Description Diagramme montrant la réflectivité radar dans de la précipitation fondant en altitude. Le pic de retour est appelé la bande brillante et est dû à une simultanéité d'un large diamètre des flocons mouillés et de la constante diélectrique plus importante de l'eau sur ces flocons.
Date Original date 13 february 2007 in German with French corrected version 2008-07-26. The diagram has as the same line as the reference now. (Reference: Frédéric Fabry of McGill University. Vertical profiles of reflectivity and precipitation intensity. UNESCO. Archived from the original on 2009-06-01. Retrieved on 28 July 2008.)
Source Modification of de:Datei:Brightband wiki.png
Author Original Averse alias Charly Whisky, French version Pierre_cb
Other versions None in Commons but de:Datei:Brightband wiki.svg in German

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I, the copyright holder of this work, hereby publish it under the following licenses:
GNU head Permission is granted to copy, distribute and/or modify this document under the terms of the GNU Free Documentation License, Version 1.2 or any later version published by the Free Software Foundation; with no Invariant Sections, no Front-Cover Texts, and no Back-Cover Texts. A copy of the license is included in the section entitled GNU Free Documentation License.
w:en:Creative Commons
attribution share alike 		This file is licensed under the Creative Commons Attribution-Share Alike 3.0 Unported license.
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Date/TimeThumbnailDimensionsUserComment
current15:00, 5 August 2008Thumbnail for version as of 15:00, 5 August 2008383 × 501 (11 KB)Charly Whisky (talk | contribs)== Description == {{Information |Description= Diagramme omntrant la réflectivité radar dans de la précipitation fondant en altitude. Le pic de retour est appelé la bande brillante et est dû à une conjuguation d'un large diamètre des flocons mouill�
03:20, 27 July 2008Thumbnail for version as of 03:20, 27 July 2008383 × 501 (7 KB)Pierre cb (talk | contribs)== Description == {{Information |Description= Diagramme omntrant la réflectivité radar dans de la précipitation fondant en altitude. Le pic de retour est appelé la bande brillante et est dû à une conjuguation d'un large diamètre des flocons mouill�

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