| contributor author | Tripoli, Gregory J. | |
| contributor author | Cotton, William R. | |
| date accessioned | 2017-06-09T16:07:13Z | |
| date available | 2017-06-09T16:07:13Z | |
| date copyright | 1989/02/01 | |
| date issued | 1989 | |
| identifier issn | 0027-0644 | |
| identifier other | ams-61376.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4202150 | |
| description abstract | The interaction of topographically induced thermally and mechanically driven diurnal flow regimes in the lee of the Rockies is shown to lead to the growth of a mesoscale convective system (MCS). An organic MCS observed during the 1977 combined South Park Area Cumulus Experiment and High Plains Experiment is numerically simulated with a two-dimensional nonhydrostatic cloud model covering spatial scales of 1000 km. In this numerical investigation,meso?-, meso?- and mesoα-scales of motion are represented simultaneously. As a result, interesting features of cloud-mesoscale interaction are predicted that cannot be represented in cloud parameterization frameworks. Based on the results of this simulation, a six-stage conceptual model of orogenic development is given. | |
| publisher | American Meteorological Society | |
| title | Numerical Study of an Observed Orogenic Mesoscale Convective System. Part 1: Simulated Genesis and Comparison with Observations | |
| type | Journal Paper | |
| journal volume | 117 | |
| journal issue | 2 | |
| journal title | Monthly Weather Review | |
| identifier doi | 10.1175/1520-0493(1989)117<0273:NSOAOO>2.0.CO;2 | |
| journal fristpage | 273 | |
| journal lastpage | 304 | |
| tree | Monthly Weather Review:;1989:;volume( 117 ):;issue: 002 | |
| contenttype | Fulltext | |
