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| 001 | 9.949867 |
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| 003 | CaOODSP |
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| 005 | 20250408083227 |
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| 006 | m o d f |
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| 007 | cr bn||||||||| |
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| 008 | 250408e19520506onc ob f000 0 eng d |
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| 040 | |aCaOODSP|beng|erda|cCaOODSP |
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| 086 | 1 |aEn57-56/114-1952E-PDF |
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| 100 | 1 |aClodman, J. |q(Joseph), |d1917- |eauthor. |
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| 245 | 14|aThe current status of the theory of pressure change with particular reference to the steering of surface lows / |cby Joseph Clodman. |
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| 264 | 1|a[Toronto] : |bMeteorological Division - Department of Transport - Canada, |c6 May 52. |
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| 300 | |a1 online resource (18 pages). |
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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 ; |v114 |
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| 500 | |aCaption title. |
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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 17-18). |
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| 520 | |a"For some time practicing forecasters have been utilizing upper air flow as an indication of the motion of surface pressure centres. Lately there have been some doubts cast on this technique both on an empirical and a theoretical basis. Although there may be some validity to these criticisms, the forecasters who have made judicious use of this method will hesitate to discard it because of its proven value, particularly where other indications of motion are obscure or non-existent"--Introduction, page 2. |
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| 650 | 0|aLows (Meteorology)|xMathematical models. |
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| 650 | 0|aForecasting|xMathematical models. |
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| 650 | 0|aForecasting|xMethodology. |
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| 650 | 6|aDépressions barométriques|xModèles mathématiques. |
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| 650 | 6|aPrévision|xModèles mathématiques. |
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| 650 | 6|aPrévision|xMeĢthodologie. |
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| 710 | 1 |aCanada. |bMeteorological Division, |eissuing body. |
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| 830 | #0|aTEC ;|v114.|w(CaOODSP)9.934253 |
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| 856 | 40|qPDF|s746 KB|uhttps://publications.gc.ca/collections/collection_2025/eccc/en57/En57-56-114-1952-eng.pdf |
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| 986 | |a672572425|aCIR-2101 |
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