HIGH LEVEL VERTICAL MOTION IN RELATION TO TROPICAL RAINFALLSource: Monthly Weather Review:;1953:;volume( 081 ):;issue: 010::page 319Author:MILLER, BANNER I.
DOI: 10.1175/1520-0493(1953)081<0319:HLVMIR>2.0.CO;2Publisher: American Meteorological Society
Abstract: A single-station technique is used to compute vertical velocities over San Juan, P. R., at standard constant pressure levels from 850 to 100 mb. Periods of strong upward motion are observed to occur rather frequently within the layer 400 to 100 mb. and these are discussed in relation to subsequent precipitation patterns.
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| contributor author | MILLER, BANNER I. | |
| date accessioned | 2017-06-09T15:55:09Z | |
| date available | 2017-06-09T15:55:09Z | |
| date copyright | 1953/10/01 | |
| date issued | 1953 | |
| identifier issn | 0027-0644 | |
| identifier other | ams-56702.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4196957 | |
| description abstract | A single-station technique is used to compute vertical velocities over San Juan, P. R., at standard constant pressure levels from 850 to 100 mb. Periods of strong upward motion are observed to occur rather frequently within the layer 400 to 100 mb. and these are discussed in relation to subsequent precipitation patterns. | |
| publisher | American Meteorological Society | |
| title | HIGH LEVEL VERTICAL MOTION IN RELATION TO TROPICAL RAINFALL | |
| type | Journal Paper | |
| journal volume | 81 | |
| journal issue | 10 | |
| journal title | Monthly Weather Review | |
| identifier doi | 10.1175/1520-0493(1953)081<0319:HLVMIR>2.0.CO;2 | |
| journal fristpage | 319 | |
| journal lastpage | 325 | |
| tree | Monthly Weather Review:;1953:;volume( 081 ):;issue: 010 | |
| contenttype | Fulltext |