00000nam 2200000za 4500 9.868848 CaOODSP 20241203113646 m go d f cr ||||||||||| 190225e19811005bcca|||fo| f000 0 eng d CaOODSP eng CaOODSP rda n-cn-bc En57-44/81-021E-PDF Spagnol, John, author. The upslope effect? / John Spagnol, satellite development meteorologist. Vancouver : Pacific Weather Centre, October 5, 1981. 1 online resource (3 pages, 2 unnumbered pages) : illustrations text txt rdacontent computer c rdamedia online resource cr rdacarrier Pacific region technical notes ; no. 81-021 Digitized edition from print [produced by Environment and Climate Change Canada]. Caption title. "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." gccst Weather forecasts gccst Precipitation gccst Wind Canada. Environment Canada. Canada. Atmospheric Environment Service. Pacific Region. Canada. Atmospheric Environment Service. Pacific Weather Center. Pacific region technical notes (Canada. Atmospheric Environment Service. Pacific Region) no. 81-021 (CaOODSP)9.865532 PDF 346 KB https://publications.gc.ca/collections/collection_2019/eccc/en57-44/En57-44-81-021-eng.pdf