| 000 | 00000nam 2200000za 4500 |
| 001 | 9.868871 |
| 003 | CaOODSP |
| 005 | 20241203113646 |
| 006 | m go d f |
| 007 | cr ||||||||||| |
| 008 | 190226e19811126bcca|||fo| f000 0 eng d |
| 040 | |aCaOODSP|beng|cCaOODSP|erda |
| 043 | |an-cn-bc |
| 086 | 1 |aEn57-44/81-027E-PDF |
| 100 | 1 |aMorin, Pat, |eauthor. |
| 245 | 10|aWindstorm over southwestern B.C. Saturday November 14, 1981 / |cPat Morin, supervising meteorologist. |
| 264 | 1|aVancouver : |bPacific Weather Centre, |cNovember 26, 1981. |
| 300 | |a1 online resource (4 pages, 5 unnumbered pages) : |billustrations |
| 336 | |atext|btxt|2rdacontent |
| 337 | |acomputer|bc|2rdamedia |
| 338 | |aonline resource|bcr|2rdacarrier |
| 490 | 1 |aPacific region technical notes ; |vno. 81-027 |
| 500 | |aDigitized edition from print [produced by Environment and Climate Change Canada]. |
| 500 | |aCaption title. |
| 504 | |aIncludes bibliographical references (pages 3-4). |
| 520 | 0 |a"A windstorm which moved up the U.S. west coast and into Southwestern B.C. caused extensive power outages over Southern B.C. on November 14, 1981. An examination of three-hourly synoptic data during the period indicates that the strong winds were due to the following factors: (1) a strong east-west pressure gradient; (2) an unusually high isallobaric gradient; (3) the funelling effect of the Olympics and the Cascade Range." |
| 692 | 07|2gccst|aWeather forecasts |
| 692 | 07|2gccst|aWind |
| 710 | 1 |aCanada. |bEnvironment Canada. |
| 710 | 1 |aCanada. |bAtmospheric Environment Service. |bPacific Region. |
| 710 | 1 |aCanada. |bAtmospheric Environment Service. |bPacific Weather Center. |
| 830 | #0|aPacific region technical notes (Canada. Atmospheric Environment Service. Pacific Region)|vno. 81-027|w(CaOODSP)9.865532 |
| 856 | 40|qPDF|s1.19 MB|uhttps://publications.gc.ca/collections/collection_2019/eccc/en57-44/En57-44-81-027-eng.pdf |