| 000 | 00000nam 2200000zi 4500 |
| 001 | 9.949310 |
| 003 | CaOODSP |
| 005 | 20250320085845 |
| 006 | m o d f |
| 007 | cr bn||||||||| |
| 008 | 250320e19470625oncb o f000 0 eng d |
| 040 | |aCaOODSP|beng|erda|cCaOODSP |
| 043 | |an-us-nc|an-gl---|an-cn-ns |
| 086 | 1 |aEn57-56/18-1947E-PDF |
| 100 | 1 |aDexter, R. V., |eauthor. |
| 245 | 13|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 |
| 490 | 1 |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. |
| 710 | 1 |aCanada. |bMeteorological Division, |eissuing body. |
| 830 | #0|aTEC ;|v18.|w(CaOODSP)9.934253 |
| 856 | 40|qPDF|s194 KB|uhttps://publications.gc.ca/collections/collection_2025/eccc/en57/En57-56-18-1947-eng.pdf |
| 986 | |a672572425|aCIR-1283 |