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| 01976nam 2200385zi 4500 |
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| 001 | 9.883916 |
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| 003 | CaOODSP |
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| 005 | 20221107170722 |
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| 006 | m o d f |
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| 007 | cr |n||||||||| |
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| 008 | 200124e197705##oncdb ob f000 0 eng d |
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| 040 | |aCaOODSP|beng|erda|cCaOODSP |
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| 041 | |aeng|bfre |
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| 043 | |ar------ |
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| 086 | 1 |aEn57-46/31E-PDF |
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| 100 | 1 |aFindlay, B. F., |eauthor. |
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| 245 | 10|aClimatic aspects of sub-polar regions / |cby B.F. Findlay and R.A. Treidl. |
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| 264 | 1|aToronto : |bAtmospheric Environment Service, Meteorological Applications Branch, |cMay 1977. |
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| 300 | |a1 online resource (25 pages, 20 unnumbered pages) : |bcharts, maps. |
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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 |aProject report (Canada. Meteorological Applications Branch) ; |vno. 31 |
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| 500 | |aDigitized edition from print [produced by Environment and Climate Change Canada]. |
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| 504 | |aIncludes bibliographical references (pages 23-25). |
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| 520 | 3 |a"In global terms sub-polar land masses are, situated such that unique life zones evolve from weak annual regimes of insolation, low temperature, and meagre precipitation. Though broad climatic similarities may seem to occur over vast areas, even where terrain contrasts are notable, there are important differences between the tundra and boreal forest as well as continental and maritime zones"--Abstract. |
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| 546 | |aIncludes abstract in French. |
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| 651 | 0|aArctic regions|xClimate. |
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| 651 | 6|aArctique|xClimat. |
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| 710 | 1 |aCanada. |bEnvironment Canada. |
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| 710 | 1 |aCanada. |bAtmospheric Environment Service. |
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| 710 | 1 |aCanada. |bMeteorological Applications Branch. |
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| 830 | #0|aProject report (Canada. Meteorological Applications Branch)|vno. 31.|w(CaOODSP)9.883702 |
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| 856 | 40|qPDF|s74.36 MB|uhttps://publications.gc.ca/collections/collection_2020/eccc/En57-46-31-eng.pdf |
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