| 000 | 00000nam 2200000zi 4500 |
| 001 | 9.952817 |
| 003 | CaOODSP |
| 005 | 20250627134537 |
| 006 | m o d f |
| 007 | cr bn||||||||| |
| 008 | 250627e19620309oncd ob f000 0 eng d |
| 040 | |aCaOODSP|beng|erda|cCaOODSP |
| 043 | |an------ |
| 086 | 1 |aEn57-56/400-1962E-PDF |
| 100 | 1 |aHarley, W. S. |q(William S.)|eauthor. |
| 245 | 10|aDistributions of wet-bulb potential temperature in North American airmasses (1957) and a statistical analysis of results / |cby W.S. Harley. |
| 264 | 1|a[Toronto] : |bMeteorological Branch - Department of Transport - Canada, |c9 Mar. 62. |
| 300 | |a1 online resource (46 pages) : |bgraphs. |
| 336 | |atext|btxt|2rdacontent |
| 337 | |acomputer|bc|2rdamedia |
| 338 | |aonline resource|bcr|2rdacarrier |
| 490 | 1 |aTEC ; |v400 |
| 500 | |aCover title. |
| 500 | |aDigitized edition from print [produced by Environment and Climate Change Canada]. |
| 504 | |aIncludes bibliographical references (pages 24-25). |
| 520 | |a"This study, among others, has shown that the Frontal Contour model can be applied over a large landmass subject to periodic outbreaks of airmasses of contrasting properties. It may also be applied with advantage in Maritime regions where there is a fairly dense network of radiosonde stations"--Conclusion, page 23. |
| 650 | 0|aWet-bulb thermometers. |
| 650 | 0|aAir masses|zNorth America. |
| 650 | 0|aAtmospheric temperature|zNorth America|xStatistical methods. |
| 650 | 6|aThermomètres mouillés. |
| 650 | 6|aMasses d'air|zAmérique du Nord. |
| 650 | 6|aTempérature atmosphérique|zAmérique du Nord|xMéthodes statistiques. |
| 710 | 1 |aCanada. |bMeteorological Branch, |eissuing body. |
| 830 | #0|aTEC ;|v400.|w(CaOODSP)9.934253 |
| 856 | 40|qPDF|s2.40 MB|uhttps://publications.gc.ca/collections/collection_2025/eccc/en57/En57-56-400-1962-eng.pdf |
| 986 | |a672572426|aCIR-3622|aUDC: 551.513.2 |