The upslope effect? / John Spagnol, satellite development meteorologist.: En57-44/81-021E-PDF
"For many years, meteorologists have noticed that accumulated precipitation on the windward side of a mountain chain was greater than that on the lee side of the same mountains. Most textbook explanation of this phenomenon are usually referred to as the classical 'orographic upslope effect' ... The remainder of the note developms another possible explanation for the orographic effect."
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Department/Agency | Canada. Environment Canada. Canada. Atmospheric Environment Service. Pacific Region. Canada. Atmospheric Environment Service. Pacific Weather Center. |
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Title | The upslope effect? / John Spagnol, satellite development meteorologist. |
Series title | Pacific region technical notes ; no. 81-021 |
Publication type | Series - View Master Record |
Language | [English] |
Format | Electronic |
Electronic document | |
Note(s) | Digitized edition from print [produced by Environment and Climate Change Canada]. Caption title. |
Publishing information | Vancouver : Pacific Weather Centre, October 5, 1981. |
Author / Contributor | Spagnol, John, author. |
Description | 1 online resource (3 pages, 2 unnumbered pages) : illustrations |
Catalogue number |
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Subject terms | Weather forecasts Precipitation Wind |
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