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| 02040cam 2200373za 4500 |
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| 001 | 9.868348 |
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| 003 | CaOODSP |
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| 005 | 20221107162548 |
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| 006 | m go d f |
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| 007 | cr ||||||||||| |
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| 008 | 190214e19790214bcca|||fo f000 0 eng d |
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| 040 | |aCaOODSP|beng|cCaOODSP|erda |
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| 043 | |an-cn-bc |
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| 086 | 1 |aEn57-44/79-004E-PDF |
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| 100 | 1 |aSpagnol, John, |eauthor. |
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| 245 | 10|aRelationship of cloudy systems to wind and vorticity fields / |cJohn Spagnol, meteorologist. |
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| 264 | 1|a[Vancouver] : |bPacific Weather Centre, |cFebruary 14, 1979. |
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| 300 | |a1 online resource (5 unnumbered pages) : |billustrations |
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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 |aPacific region technical notes ; |vno. 79-004 |
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| 500 | |aCaption title. |
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| 500 | |aDigitized edition from print [produced by Environment and Climate Change Canada]. |
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| 504 | |aIncludes bibliographical references. |
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| 520 | |a"Since one of the main forecast tools is the computer forecast of the 500 mb height field (with vorticity analysis of the wind field), it is important that the P/A be convinced that the initial field over the Pacific is accurate. This is best accomplished by use of the most reliable source of information over the Pacific--the GOES satellite image. The cloud formations seen on the satellite pictures are compared with the vorticity and height fields as seen on the analysis." |
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| 692 | 07|2gccst|aWeather forecasts |
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| 692 | 07|2gccst|aSatellite imagery |
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| 710 | 1 |aCanada. |bEnvironment Canada. |
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| 710 | 1 |aCanada. |bAtmospheric Environment Service. |bPacific Region. |
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| 710 | 1 |aCanada. |bAtmospheric Environment Service. |bPacific Weather Center. |
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| 830 | #0|aPacific region technical notes (Canada. Atmospheric Environment Service. Pacific Region)|vno. 79-004|w(CaOODSP)9.865532 |
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| 856 | 40|qPDF|s774 KB|uhttps://publications.gc.ca/collections/collection_2019/eccc/en57-44/En57-44-79-004-eng.pdf |
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