File:Annotated Skew T diagram.png
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Summary
| Description |
English: The altitude of clouds can be partially inferred by high relative humidity, where the dewpoint and temperature are close. The type of cloud is suggested by the stability of the atmosphere, determined by the steepness of the temperature profile compared to the adiabatic lapse rate. The underlying graph was downloaded from the University of Wyoming atmospheric soundings archive, http://weather.uwyo.edu/upperair/sounding.html. |
| Date | |
| Source | Own work |
| Author | JeanBizHertzberg |
| Other versions | Derivative works of this file: Skew T annoté.png |
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 23:47, 27 October 2022 | | 864 × 720 (97 KB) | JeanBizHertzberg | Uploaded own work with UploadWizard |
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