| 000 | 00000nam 2200000zi 4500 |
| 001 | 9.957026 |
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| 003 | CaOODSP |
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| 005 | 20251103133809 |
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| 006 | m o d f |
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| 007 | cr bn||||||||| |
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| 008 | 251103e19641013oncdb ob f000 0 eng d |
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| 040 | |aCaOODSP|beng|erda|cCaOODSP |
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| 043 | |an-cn--- |
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| 086 | 1 |aEn57-56/541-1964E-PDF |
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| 100 | 1 |aSeale, David, |eauthor. |
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| 245 | 14|aThe diurnal variation of wind in the lowest 5000 feet / |cby David Seale. |
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| 264 | 1|a[Toronto, Ontario] : |bDepartment of Transport, Meteorological Branch, |cOctober 13, 1964. |
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| 300 | |a1 online resource (4 pages, 6 unnumbered pages) : |bcharts, map. |
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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 |aTEC ; |v541 |
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| 500 | |aDigitized edition from print [produced by Environment and Climate Change Canada]. |
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| 500 | |a"CIR 4126." |
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| 504 | |aIncludes bibliographical references (page 4). |
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| 520 | 3 |a"The variation of wind with height up to 5000 ft above terrain for morning and afternoon observations is discussed. The wind profiles of five days were averaged and compared to the wind at 5000 ft. The depth of the layer of frictional influence was found to be about 2000 ft in the morning and 3000 ft in the afternoon. A pronounced maximum in the ratio of morning to afternoon wind speeds was noted at about 1000 ft"--Abstract. |
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| 650 | 0|aWinds|xSpeed|zCanada|xMeasurement. |
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| 650 | 6|aVents|xVitesse|zCanada|xMesure. |
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| 710 | 1 |aCanada. |bMeteorological Branch, |eissuing body. |
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| 830 | #0|aTEC ;|v541.|w(CaOODSP)9.934253 |
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| 856 | 40|qPDF|s367 KB|uhttps://publications.gc.ca/collections/collection_2025/eccc/en57/En57-56-541-1964-eng.pdf |
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| 986 | |aU.D.C. 551.557.31 |
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