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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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Captions

Skew T diagrams can suggest where and what type of clouds are present.

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inception

27 October 2022

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image/png

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1082f3034d9957bf4972e61e40203ad4b7fd0887

determination method or standard: SHA-1

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99,281 byte

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720 pixel

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864 pixel

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Date/TimeThumbnailDimensionsUserComment
current23:47, 27 October 2022Thumbnail for version as of 23:47, 27 October 2022864 × 720 (97 KB)JeanBizHertzbergUploaded own work with UploadWizard

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