File:Skew T annoté.png
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Français : L'altitude des nuages peut être partiellement déduite d'une humidité relative élevée, où le point de rosée et la température sont proches. Le type de nuage est suggéré par la stabilité de l'atmosphère, déterminée par l'inclinaison du profil de température par rapport au taux de déclin adiabatique. Le graphique sous-jacent a été téléchargé à partir des archives de sondages atmosphériques de l'Université du Wyoming, http://weather.uwyo.edu/upperair/sounding.html |
| Date | |
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This file was derived from: Annotated Skew T diagram.png |
| Author | Pierre cb |
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I, the copyright holder of this work, hereby publish it under the following license:
This file is licensed under the Creative Commons Attribution 4.0 International license.
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 11:13, 2 June 2024 | | 857 × 703 (107 KB) | Pierre cb (talk | contribs) | Petite correction |
| 11:09, 2 June 2024 |  | 857 × 703 (103 KB) | Pierre cb (talk | contribs) | Meilleure version | |
| 17:32, 31 May 2024 |  | 864 × 720 (96 KB) | Pierre cb (talk | contribs) | Uploaded own work with UploadWizard |
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