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040 |aCaOODSP|beng|erda|cCaOODSP
041 |aeng|beng|bfre
0861 |aEn57-56/614-1966E-PDF
1001 |aCampbell, John, |eauthor.
24510|aExtreme values of the terms neglected in the vorticity equation / |cby John Campbell and David Davies.
24633|aValeurs extrêmes des termes négligés dans l'équation de tourbillon
264 1|aToronto, Ontario : |bDepartment of Transport, Meteorological Branch, |cApr. 16, 1966.
300 |a1 online resource (46 pages, 2 unnumbered pages) : |bmaps.
336 |atext|btxt|2rdacontent
337 |acomputer|bc|2rdamedia
338 |aonline resource|bcr|2rdacarrier
4901 |aTEC ; |v614
500 |aDigitized edition from print [produced by Environment and Climate Change Canada].
500 |a"CIR 4416."
504 |aIncludes bibliographical references (page 13).
5203 |a"For each of three synoptic situations, all the terms, in the vorticity equation are computed at 1000, 850, 700, and 500 mb. When the results based on diagnostic vertical motion fields are studied in some detail, they show that the terms neglected in the Central Analysis Office baroclinic model attain their maximum magnitude in the neighbourhood of developing disturbances. In these regions, especially at 1000mb, their sum may approach or exceed that of the terms retained"--Abstract.
546 |aText in English; abstract in English and French.
650 0|aBaroclinic models.
650 6|aModèles baroclines.
7101 |aCanada. |bMeteorological Branch, |eissuing body.
830#0|aTEC ;|v614.|w(CaOODSP)9.934253
85640|qPDF|s1540 KB|uhttps://publications.gc.ca/collections/collection_2025/eccc/en57/En57-56-614-1966-eng.pdf
986 |aU.D.C. 551.509.313