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The depth of the marine layer at San Diego as related to subsequent cool season precipitation episodes in Arizona
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1979
[PDF-1.47 MB]
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Description:The relationship between the depth of the marine layer at San Diego, California, and potential precipitation episodes in Arizona during the cool season is studied. It is shown that a marine layer from the surface to at least the 700-mb level is generally necessary for consideration of a subsequent widespread precipitation episode in Arizona. The relationship of the height of this marine inversion to the current vertical motion field is also discussed.
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Content Notes:Includes bibliographical references (page 7).
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Rights Information:Public Domain
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Compliance:Library
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