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008251103s1965    oncb    ob   f000 0 eng d
040 |aCaOODSP|beng|erda|cCaOODSP
041 |aeng|beng|bfre
0861 |aEn57-56/551-1965E-PDF
1001 |aKruger, H. B., |eauthor.
24510|aEstimates of 1000-mb height and temperature changes from surface synoptic data / |cby H.B. Kruger & C. Marullo.
24636|aEstimates of 1000-mb height and temperature from surface synoptic data
24633|aEstimation de la hauteur et de la température a 1,000 mb à l'aide de données synoptiques de surface
264 1|aToronto, Ontario : |bDepartment of Transport, Meteorological Branch, |c1965.
300 |a1 online resource (13 pages, 3 unnumbered pages) : |bmap.
336 |atext|btxt|2rdacontent
337 |acomputer|bc|2rdamedia
338 |aonline resource|bcr|2rdacarrier
4901 |aTEC ; |v551
500 |aDigitized edition from print [produced by Environment and Climate Change Canada].
500 |a"21 Jan. 65."
500 |a"CIR 4173."
504 |aIncludes bibliographical references (page 8).
5203 |a"Several formulas for calculating 1000-mb height and temperature from regular synoptic reports of surface temperature and sea-level pressure are evaluated. The results indicate that a version of the hypsometric formula can be used to calculate a 1000-mb height comparable to the reported value, while application of an appropriate lapse rate to the observed surface temperature seems to be an acceptable method of estimating the corresponding 1000-mb temperature. A possible application of these results in an objective analysis scheme is discussed briefly"--Abstract.
546 |aText in English; abstract in English and French.
650 0|aUpper air temperature|xMeasurement.
650 6|aTempérature en altitude|xMesure.
7101 |aCanada. |bMeteorological Branch, |eissuing body.
830#0|aTEC ;|v551.|w(CaOODSP)9.934253
85640|qPDF|s795 KB|uhttps://publications.gc.ca/collections/collection_2025/eccc/en57/En57-56-551-1965-eng.pdf
986 |aU.D.C. 551.509.313 :551.509.323.7