File:SeaBreeze-fr.svg

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Summary

Description
English: Schematic cross section through a sea breeze front. If the air inland is moist, cumulus often marks the front.
Français : Le réchauffement de l'air au-dessus de la terre est plus rapide que celui au-dessus de la mer suite à la différence de capacité thermique entre les deux milieux. Par ciel clair de jour, il s'en suit un flux d'air qui est montré sur ce diagramme. L'air chaud étant moins dense peut être repoussé en altitude par l'air plus frais venant de la mer le long du front de brise de mer. Ce denier sera le plus souvent visible grâce à la présence de nuages convectifs, de types cumulus, si l'air chaud est assez humide. En aval et en amont de ce front se trouvent par contre des zones de subsidence de l'air et donc un ciel généralement dégagé.
Date (UTC)
Source SeaBreeze.svg
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SeaBreeze.svg, SeaBreeze.jpg: U.S. FAA AC 00-6A, Chapter 16, Figure 165.

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This is a retouched picture, which means that it has been digitally altered from its original version. Modifications: Translation in French. The original can be viewed here: SeaBreeze.svg. Modifications made by M0tty.

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  • File:SeaBreeze.svg licensed with PD-self
    • 2011-10-17T08:05:19Z Malyszkz 441x264 (26974 Bytes) == {{int:filedesc}} == {{Information |Description={{en|Schematic cross section through a sea breeze front. If the air inland is moist, cumulus often marks the front.}} |Source=*[[:File:SeaBreeze.jpg|]] |Date=2011-10-17 08:04

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21 October 2011

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Date/TimeThumbnailDimensionsUserComment
current19:59, 21 October 2011Thumbnail for version as of 19:59, 21 October 2011441 × 264 (26 KB)M0ttycorr "froid" -> "frais"
19:54, 21 October 2011Thumbnail for version as of 19:54, 21 October 2011441 × 264 (26 KB)M0tty== {{int:filedesc}} == {{Information |Description={{en|Schematic cross section through a sea breeze front. If the air inland is moist, cumulus often marks the front.}} |Source=*File:SeaBreeze.svg |Date=2011-10-21 19:53 (UTC) |Author=*[[:File:SeaBree
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