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| 02090nam 2200361za 4500 |
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| 001 | 9.868899 |
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| 003 | CaOODSP |
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| 005 | 20221107162719 |
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| 006 | m go d f |
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| 007 | cr ||||||||||| |
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| 008 | 190226e19820601bcca|||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 |aEn57-44/82-005E-PDF |
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| 100 | 1 |aGrimes, David, |eauthor. |
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| 245 | 10|aFourier analysis for Hovmöller program at PWC / |cDavid Grimes, supervising meteorologist. |
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| 264 | 1|aVancouver, B.C. : |bPacific Weather Centre, |cJune 1, 1982. |
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| 300 | |a1 online resource (4 pages, 4 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. 82-005 |
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| 500 | |aDigitized edition from print [produced by Environment and Climate Change Canada]. |
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| 500 | |aCaption title. |
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| 504 | |aIncludes bibliographical references (page 4). |
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| 520 | 0 |a"Over the winter months Hovmöller data has been collected and analyzed in a variety of formats. 500 millibar height datas is averaged over a latitude band for every 5 degrees of longitude. The conventional method of displaying this data has been in a X-T diagram referred to today as the Hovmöller diagram. ... The method of analyzing the wave forms on this particular diagram is the subject of another report and will not be discussed here. However, harmonic analysis has been a popular tool for deciphering the significant wave patterns in the data." |
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| 692 | 07|2gccst|aWeather forecasts |
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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. 82-005|w(CaOODSP)9.865532 |
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| 856 | 40|qPDF|s886 KB|uhttps://publications.gc.ca/collections/collection_2019/eccc/en57-44/En57-44-82-005-eng.pdf |
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