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040 |aCaOODSP|beng|erda|cCaOODSP
043 |an-us-nc|an-gl---|an-cn-ns
0861 |aEn57-56/18-1947E-PDF
1001 |aDexter, R. V., |eauthor.
24513|aAn aid to forecasting precipitation from the Hatteras Low / |cby R.V. Dexter.
264 1|a[Toronto] : |bMeteorological Division - Department of Transport - Canada, |c25 Jun 47.
300 |a1 online resource (3 pages, 1 unnumbered page) : |bmaps.
336 |atext|btxt|2rdacontent
337 |acomputer|bc|2rdamedia
338 |aonline resource|bcr|2rdacarrier
4901 |aTEC ; |v18
500 |aCaption title.
500 |aDigitized edition from print [produced by Environment and Climate Change Canada].
520 |a"Consideration of the synoptic charts for the year 1946 shows a relation between the position of the centre of a depression near Iceland at the time of first appearance of a Hatteras Low and the subsequent behavior of the latter. It is possible to define an area near Greenland, such that the presence of the centre of a depression within it indicates that the Hatteras Low will subsequently cause precipitation in Nova Scotia. The overall accuracy of this method of forecasting precipitation or no precipitation is 80% for the year 1946"--Summary, page [1].
650 0|aLows (Meteorology)|zNorth Carolina|zHatteras, Cape.
650 0|aLows (Meteorology)|zGreenland.
650 0|aPrecipitation forecasting|zNova Scotia.
650 6|aDépressions barométriques|zCaroline du Nord|zHatteras, Cap.
650 6|aDépressions barométriques|zGroenland.
650 6|aPrécipitations (Météorologie)|xPrévision|zNouvelle-Écosse.
7101 |aCanada. |bMeteorological Division, |eissuing body.
830#0|aTEC ;|v18.|w(CaOODSP)9.934253
85640|qPDF|s194 KB|uhttps://publications.gc.ca/collections/collection_2025/eccc/en57/En57-56-18-1947-eng.pdf
986 |a672572425|aCIR-1283