| 000 | 00000nam 2200000zi 4500 |
| 001 | 9.956395 |
| 003 | CaOODSP |
| 005 | 20251016160852 |
| 006 | m o d f |
| 007 | cr bn||||||||| |
| 008 | 251016s1962 oncbd ob f000 0 eng d |
| 040 | |aCaOODSP|beng|erda|cCaOODSP |
| 043 | |an-cn-bc |
| 086 | 1 |aEn57-56/430-1962E-PDF |
| 100 | 1 |aHarms, A. A, |eauthor. |
| 245 | 13|aAn empirical method for the prediction of breaks in hot spells at Vancouver / |cby A.A. Harms and D.C. Healey. |
| 264 | 1|a[Toronto, Ontario] : |bMeteorological Branch, Department of Transport, |c1962. |
| 300 | |a1 online resource (35 pages, 2 unnumbered pages) : |bmaps, charts. |
| 336 | |atext|btxt|2rdacontent |
| 337 | |acomputer|bc|2rdamedia |
| 338 | |aonline resource|bcr|2rdacarrier |
| 490 | 1 |aTEC ; |v430 |
| 500 | |aDigitized edition from print [produced by Environment and Climate Change Canada]. |
| 500 | |a"1 Nov. 62." |
| 500 | |a"CIR 3748." |
| 504 | |aIncludes bibliographical references (page 12). |
| 520 | |a"A formula making it possible to determine the deviation in the monthly mean sea level at Vancouver and other B.C. coastal stations on the basis of mean pressure and prevailing wind is derived. A formula of similar form is then applied to the errors in individual tidal predictions, and its limitations discussed. A summary of the characteristics of a number of storm surges and the associated "lows" is also included"--Abstract. |
| 650 | 0|aTemperature|zBritish Columbia|zVancouver. |
| 650 | 0|aTemperature measurements|zBritish Columbia|zVancouver. |
| 650 | 6|aTempérature|zColombie-Britannique|zVancouver. |
| 650 | 6|aThermométrie|zColombie-Britannique|zVancouver. |
| 651 | 0|aVancouver (B.C.)|xClimate. |
| 651 | 6|aVancouver (C.-B.)|xClimat. |
| 710 | 1 |aCanada. |bMeteorological Branch, |eissuing body. |
| 830 | #0|aTEC ;|v430.|w(CaOODSP)9.934253 |
| 856 | 40|qPDF|s1654 KB|uhttps://publications.gc.ca/collections/collection_2025/eccc/en57/En57-56-430-1962-eng.pdf |
| 986 | |aUDC: 551.509.323. |