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| 001 | 9.956934 |
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| 003 | CaOODSP |
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| 005 | 20251030164232 |
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| 006 | m o d f |
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| 007 | cr bn||||||||| |
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| 008 | 251030s1964 oncd ob f000 0 eng d |
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| 040 | |aCaOODSP|beng|erda|cCaOODSP |
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| 043 | |aln----- |
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| 086 | 1 |aEn57-56/521-1964E-PDF |
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| 100 | 1 |aJarvis, E. C., |eauthor. |
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| 245 | 14|aThe diabatic contribution to thickness tendency / |cby E.C. Jarvis. |
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| 264 | 1|a[Toronto, Ontario] : |bDepartment of Transport, Meteorological Branch, |c1964. |
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| 300 | |a1 online resource (12 pages, 4 unnumbered pages) : |bcharts. |
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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 |aTEC ; |v521 |
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| 500 | |aDigitized edition from print [produced by Environment and Climate Change Canada]. |
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| 500 | |a"25 May 64." |
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| 500 | |a"CIR 4042." |
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| 504 | |aIncludes bibliographical references (pages 11-12). |
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| 520 | 3 |a"Important diabatic processes occurring in the atmosphere are briefly discussed and their contribution to thickness change is calculated for selected stations on the North Atlantic Ocean during a seven-day winter period. Results are compared with the diabatic thickness change determined by evaluating the terms in the thickness tendency equation. Although measurement errors are appreciable, values obtained by the two methods are comparable when the data have been suitably smoothed. The results indicate the fiux of sensible heat and water vapour can be used to evaluate the diabatic contribution to thickness tendency when cold air advection is occurring over the sea"--Abstract. |
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| 650 | 0|aBoundary layer (Meteorology)|zNorth Atlantic Ocean. |
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| 650 | 6|aCouche limite (Météorologie)|zAtlantique Nord. |
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| 651 | 0|aNorth Atlantic Ocean|xClimate. |
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| 651 | 6|aAtlantique Nord|xClimat. |
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| 710 | 1 |aCanada. |bMeteorological Branch, |eissuing body. |
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| 830 | #0|aTEC ;|v521.|w(CaOODSP)9.934253 |
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| 856 | 40|qPDF|s792 KB|uhttps://publications.gc.ca/collections/collection_2025/eccc/en57/En57-56-521-1964-eng.pdf |
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| 986 | |aU.D.C. 551.511.33 :551.510.522 :551.524.4 |
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