| 000 | 00000nam 2200000zi 4500 |
| 001 | 9.957165 |
| 003 | CaOODSP |
| 005 | 20251106144352 |
| 006 | m o d f |
| 007 | cr bn||||||||| |
| 008 | 251106e19660210oncd ob f000 0 eng d |
| 040 | |aCaOODSP|beng|erda|cCaOODSP |
| 041 | |aeng|beng|bfre |
| 043 | |an-cn-ab |
| 086 | 1 |aEn57-56/598-1966E-PDF |
| 100 | 1 |aWebb, M. S. |q(Michael S.)|eauthor. |
| 245 | 13|aAn approach to forecasting low surface humidities at night in the Rocky Mountains / |cby M.S. Webb. |
| 246 | 33|aMéthode de prévision des faibles humidités de surface, la nuit, dans les montagnes rocheuses |
| 264 | 1|aToronto, Ontario : |bDepartment of Transport, Meteorological Branch, |cFeb. 10, 1966. |
| 300 | |a1 online resource (9 pages, 2 unnumbered pages) : |bcharts. |
| 336 | |atext|btxt|2rdacontent |
| 337 | |acomputer|bc|2rdamedia |
| 338 | |aonline resource|bcr|2rdacarrier |
| 490 | 1 |aTEC ; |v598 |
| 500 | |aDigitized edition from print [produced by Environment and Climate Change Canada]. |
| 500 | |a"CIR 4377." |
| 504 | |aIncludes bibliographical references (page 9). |
| 520 | 3 |a"Low surface relative humidities at night in the Rocky Mountains can increase significantly the flammability of forested areas. Through examination of the wind and temperature characteristics of the air stream aloft, an approach to forecasting these low humidity occurrences is presented. The extent to which the airstream characteristics favour lee wave formation during these occurrences is discussed"--Abstract. |
| 546 | |aText in English; abstract in English and French. |
| 650 | 0|aHumidity|zAlberta|zKananaskis. |
| 650 | 6|aAir|xHumidité|zAlberta|zKananaskis. |
| 651 | 0|aKananaskis (Alta.)|xClimate. |
| 651 | 6|aKananaskis (Alb.)|xClimat. |
| 710 | 1 |aCanada. |bMeteorological Branch, |eissuing body. |
| 830 | #0|aTEC ;|v598.|w(CaOODSP)9.934253 |
| 856 | 40|qPDF|s460 KB|uhttps://publications.gc.ca/collections/collection_2025/eccc/en57/En57-56-598-1966-eng.pdf |
| 986 | |aU.D.C. 551.509.329 :551.509.317 |