| contributor author | Haltiner, G. J. | |
| contributor author | Wang, Yeh-chum | |
| date accessioned | 2017-06-09T14:12:19Z | |
| date available | 2017-06-09T14:12:19Z | |
| date copyright | 1960/04/01 | |
| date issued | 1960 | |
| identifier issn | 0095-9634 | |
| identifier other | ams-14613.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4150194 | |
| description abstract | A model for numerical prediction of the 1000-mb surface is developed which includes a term expressing the interchange of sensible heat between the air and the underlying surface as well as the effect of terrain-induced vertical motion. In spite of the crudeness of the non-adiabatic representation, the model shows a definite improvement over a similar adiabatic model when the two are compared in a series of prognoses. Moreover, when monthly mean isotherms may be used to represent the temperature of the underlying surface, the non-adiabatic term may be combined with the orographic term and the earth's vorticity so that there is no work added to the prognostic routine. | |
| publisher | American Meteorological Society | |
| title | NUMERICAL PROGNOSIS INCLUDING NON-ADIABATIC WARMING | |
| type | Journal Paper | |
| journal volume | 17 | |
| journal issue | 2 | |
| journal title | Journal of Meteorology | |
| identifier doi | 10.1175/1520-0469(1960)017<0207:NPINAW>2.0.CO;2 | |
| journal fristpage | 207 | |
| journal lastpage | 213 | |
| tree | Journal of Meteorology:;1960:;volume( 017 ):;issue: 002 | |
| contenttype | Fulltext | |