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| 01908cam 2200373za 4500 |
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| 001 | 9.868848 |
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| 003 | CaOODSP |
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| 005 | 20221107162710 |
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| 006 | m go d f |
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| 007 | cr ||||||||||| |
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| 008 | 190225e19811005bcca|||fo| f000 0 eng d |
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| 040 | |aCaOODSP|beng|cCaOODSP|erda |
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| 043 | |an-cn-bc |
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| 086 | 1 |aEn57-44/81-021E-PDF |
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| 100 | 1 |aSpagnol, John, |eauthor. |
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| 245 | 14|aThe upslope effect? / |cJohn Spagnol, satellite development meteorologist. |
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| 264 | 1|aVancouver : |bPacific Weather Centre, |cOctober 5, 1981. |
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| 300 | |a1 online resource (3 pages, 2 unnumbered pages) : |billustrations |
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| 336 | |atext|btxt|2rdacontent |
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| 337 | |acomputer|bc|2rdamedia |
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| 338 | |aonline resource|bcr|2rdacarrier |
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| 490 | 1 |aPacific region technical notes ; |vno. 81-021 |
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| 500 | |aDigitized edition from print [produced by Environment and Climate Change Canada]. |
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| 500 | |aCaption title. |
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| 520 | |a"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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| 692 | 07|2gccst|aWeather forecasts |
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| 692 | 07|2gccst|aPrecipitation |
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| 692 | 07|2gccst|aWind |
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| 710 | 1 |aCanada. |bEnvironment Canada. |
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| 710 | 1 |aCanada. |bAtmospheric Environment Service. |bPacific Region. |
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| 710 | 1 |aCanada. |bAtmospheric Environment Service. |bPacific Weather Center. |
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| 830 | #0|aPacific region technical notes (Canada. Atmospheric Environment Service. Pacific Region)|vno. 81-021|w(CaOODSP)9.865532 |
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| 856 | 40|qPDF|s346 KB|uhttps://publications.gc.ca/collections/collection_2019/eccc/en57-44/En57-44-81-021-eng.pdf |
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