File:Thermal High fr.svg
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Français : Coupe verticale pression versus hauteur des isohypses (surfaces isobares) dans un anticyclone thermique. Bien que la pression réduite au niveau de la mer puisse atteindre couramment des valeurs très élevées au centre d'un anticyclone thermique, un tel système a généralement une épaisseur réduite et se transforme en une dépression en altitude : en effet, on explique en météorologie que la différence de hauteur entre deux surfaces isobares sur une verticale donnée est d'autant plus forte que les températures de la couche atmosphérique comprise entre ces deux surfaces sont en moyenne plus élevées suivant cette verticale : par suite, dans un air très froid, la haute pression de surface s'amenuise lorsqu'on gagne en hauteur, jusqu'à s'inverser et finalement creuser une dépression. |
| Source | Own work |
| Author | Pierre cb |
| SVG development |  This chart was created with a text editor.  |
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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. |
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 22:05, 3 February 2020 | | 696 × 278 (1 KB) | Sarang (talk | contribs) | first version of true SVG, currently only fr language |
| 15:07, 2 November 2016 |  | 596 × 278 (36 KB) | Pierre cb (talk | contribs) | {{Information |Description ={{fr|1=Coupe verticale pression versus hauteur des isohypses (surfaces isobares) dans un anticyclone thermique. Bien que la pression réduite au niveau de la mer puisse atteindre couramment des valeurs très élevées au... |
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