| contributor author | WEXLER, RAYMOND | |
| contributor author | CHMELA, ALBERT C. | |
| contributor author | ARMSTRONG, GRAHAM M. | |
| date accessioned | 2017-06-09T15:58:35Z | |
| date available | 2017-06-09T15:58:35Z | |
| date copyright | 1967/12/01 | |
| date issued | 1967 | |
| identifier issn | 0027-0644 | |
| identifier other | ams-57917.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4198306 | |
| description abstract | Fields of mind velocity, divergence, and reflectivity were derived from Doppler radar measurements in a New England storm over a 6-hr. period. A layer of easterlies near the surface increased in depth and speed during the period. Above this layer the wind veered with height to SW and W, and then backed to SW. Changes in wind direction with time in the layer between 4 and 6 km. indicated the passage of mesoscale short wave troughs. Layers of convergence and divergence, alternating with height, appeared to be related to the mind regions. | |
| publisher | American Meteorological Society | |
| title | WIND FIELD OBSERVATIONS BY DOPPLER RADAR IN A NEW ENGLAND SNOWSTORM | |
| type | Journal Paper | |
| journal volume | 95 | |
| journal issue | 12 | |
| journal title | Monthly Weather Review | |
| identifier doi | 10.1175/1520-0493(1967)095<0929:WFOBDR>2.3.CO;2 | |
| journal fristpage | 929 | |
| journal lastpage | 935 | |
| tree | Monthly Weather Review:;1967:;volume( 095 ):;issue: 012 | |
| contenttype | Fulltext | |
