File:Diablo wind.jpg

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Summary

Description
English: The Diablo winds a the result of cold weather east of California over the Great Basin, mostly in Nevada and Utah,. Cool, high-pressure air hanging above the high desert runs in contrast to a warmer low-pressure system along the Pacific Coast, creating the pressure differential that’s the recipe for Diablo winds. It is first a katabatic wind descending the Sierra Nevada, then passing thru the Central Valley and finally passing over the Coastal mountains north of San Francisco it becomes a foehn wind on the other side of them.
Date
Source https://www.sfchronicle.com/environment/article/Are-infamous-Diablo-winds-responsible-for-recent-14570132.php
Author US National Weather Service of the National Oceanic and Atmospheric Administration

Licensing

Public domain
This image is in the public domain because it contains materials that originally came from the U.S. National Oceanic and Atmospheric Administration, taken or made as part of an employee's official duties.

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Captions

Explanation of the Northern California Diablo wind.

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Date/TimeThumbnailDimensionsUserComment
current17:17, 27 December 2019Thumbnail for version as of 17:17, 27 December 20191,280 × 914 (115 KB)Pierre cbUser created page with UploadWizard
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