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| 001 | 9.957066 |
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| 003 | CaOODSP |
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| 005 | 20251104115737 |
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| 006 | m o d f |
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| 007 | cr bn||||||||| |
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| 008 | 251104s1965 oncdb ob f000 0 eng d |
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| 040 | |aCaOODSP|beng|erda|cCaOODSP |
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| 041 | |aeng|beng|bfre |
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| 086 | 1 |aEn57-56/560-1965E-PDF |
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| 100 | 1 |aJarvis, E. C., |eauthor. |
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| 245 | 14|aThe application of a grid technique for forecasting frontal cyclones / |cby E.C. Jarvis. |
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| 246 | 33|aApplication d'une technique de carroyage à la prévision des cyclones frontaux |
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| 264 | 1|aToronto, Ontario : |bDepartment of Transport, Meteorological Branch, |c1965. |
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| 300 | |a1 online resource (13 pages, 43 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 |aTEC ; |v560 |
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| 500 | |aDigitized edition from print [produced by Environment and Climate Change Canada]. |
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| 500 | |a"15 Mar. 65." |
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| 500 | |a"CIR 4202." |
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| 504 | |aIncludes bibliographical references (page 13). |
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| 520 | 3 |a"A simple baroclinic prediction model has been adapted to the Wilson grid for predicting the displacement and central pressure of frontal cyclones for periods up to 24 hours. It was determined that the primary component of displacement, equivalent to the 500-mb vector wind within the area enclosed by the Wilson grid, should be adjusted for the secondary displacement resulting from the influence of sloping terrain, major diabatic processes, and the latitudinal variation of Coriolis force"--Abstract. |
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| 546 | |aText in English; abstract in English and French. |
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| 650 | 0|aCyclones. |
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| 650 | 6|aCyclones. |
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| 710 | 1 |aCanada. |bMeteorological Branch, |eissuing body. |
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| 830 | #0|aTEC ;|v560.|w(CaOODSP)9.934253 |
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| 856 | 40|qPDF|s3349 KB|uhttps://publications.gc.ca/collections/collection_2025/eccc/en57/En57-56-560-1965-eng.pdf |
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| 986 | |aU.D.C. 551.509.313 :551.509.311 |
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