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| 03320cam 2200445zi 4500 |
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001 | 9.938464 |
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003 | CaOODSP |
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005 | 20240628072857 |
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006 | m o d f |
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007 | cr bn||||||||| |
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008 | 240522s1968 oncab obt f000 0 eng d |
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040 | |aCaOODSP|beng|erda|cCaOODSP |
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041 | 0 |aeng|beng|bfre |
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043 | |an-cnp-- |
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045 | |ax6x6 |
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086 | 1 |aEn57-57/667-1968E-PDF |
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100 | 1 |aKagawa, N. H., |eauthor. |
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245 | 13|aAn evaluation of Brunt's cooling formula for minimum temperature prediction at five prairie locations / |cby N.H. Kagawa = Évaluation de la formule de refroidissement de Brunt en vue de la prédiction de la température minimale à cinq endroits des praities / par N.H. Kagawa. |
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246 | 31|aÉvaluation de la formule de refroidissement de Brunt en vue de la prédiction de la température minimale à cinq endroits des praities |
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264 | 1|aToronto, Ontario : |bCanada, Department of Transport, Meteorological Branch = Canada, Ministère des transports, Direction de la météorologie, |c1968. |
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300 | |a1 online resource (20 pages, 2 unnumbered pages) : |billustrations, map. |
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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 |aTechnical memoranda, |x0068-7804 ; |vTEC 667 |
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500 | |aISSN of series supplied from ISSN Portal. |
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500 | |a"U.D.C. 551·509·323"--Cover. |
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500 | |a"January 26, 1968"--Cover. |
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500 | |aDigitized edition from print [produced by Environment and Climate Change Canada]. |
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504 | |aIncludes bibliographical references (page 12). |
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520 | 3 |a"In this study, Brunt's equation for predicting the decrease in temperature with time after sunset is applied to the short-range prediction of minimum temperatures at five locations in Western Canada. These locations are Edmonton, Calgary, Saskatoon, Regina and Winnipeg. In order to apply Brunt's method, it was initially necessary to evaluate the product of the soil denisity, specific heat and the square root of the coefficient of termal conductivity. This was done empirically. Minimum temperature predictions were then made using data for a two month period at each of the five locations. In performing these predictions, nights during which temperature advection occurred were excluded from the test. However, cloud cover was taken into account using a scheme suggested by Reuter. Mean absolute errors between predicted and observed minimum temperatures varied from 2.3 degrees at Edmonton and Regina to 3.0 degrees at Calgary and the R.M.S. deviations ranged from 2.9 degrees at Regina to 4.0 degrees at Calgary"--Abstract. |
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546 | |aIncludes abstracts in English and French. |
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650 | 0|aAtmospheric temperature|zPrairie Provinces|xForecasting|xMathematical models|xEvaluation. |
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650 | 6|aTempérature atmosphérique|zProvinces des Prairies|xPrévision|xModèles mathématiques|xÉvaluation. |
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655 | 7|aTechnical reports|2lcgft |
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655 | 7|aRapports techniques|2rvmgf |
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710 | 1 |aCanada.|bMeteorological Branch, |eissuing body. |
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830 | #0|aTechnical memoranda (Canada. Meteorological Branch)|vTEC 667.|w(CaOODSP)9.934428 |
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856 | 40|qPDF|s739 KB|uhttps://publications.gc.ca/collections/collection_2024/eccc/en57/En57-57-667-1968-eng.pdf |
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