| dc.contributor.author | Berkofsky, Louis | |
| dc.date.accessioned | 2017-06-09T14:11:22Z | |
| dc.date.available | 2017-06-09T14:11:22Z | |
| dc.date.copyright | 1956/02/01 | |
| dc.date.issued | 1956 | |
| dc.identifier.issn | 0095-9634 | |
| dc.identifier.other | ams-14232.pdf | |
| dc.identifier.uri | http://onlinelibrary.yabesh.ir/handle/yetl/4149771 | |
| dc.description.abstract | From the premise that the modelling approximation for an integrated numerical-prediction model is given by a constraint on the stability factor in the first law of thermodynamics for adiabatic flow, a three-parameter baroclinic model is devised. The resulting flow equations contain development terms which reflect interaction between surface and 500-millibar effects. It is shown that the three-parameter model is a natural outgrowth of an attempt to render two-parameter models internally consistent. | |
| dc.publisher | American Meteorological Society | |
| dc.title | A THREE-PARAMETER BAROCLINIC NUMERICAL-PREDICTION MODEL | |
| dc.type | Journal Paper | |
| dc.journal.volume | 13 | |
| dc.journal.issue | 1 | |
| dc.journal.title | Journal of Meteorology | |
| dc.identifier.doi | 10.1175/1520-0469(1956)013<0102:ATPBNP>2.0.CO;2 | |
| dc.journal.fristpage | 102 | |
| dc.journal.lastpage | 111 | |
| dc.tree | Journal of Meteorology:;1956:;volume( 013 ):;issue: 001 | |
| dc.contenttype | Fulltext | |
