A TEST OF THE RELATION BETWEEN PRECIPITATION AND SYNOPTIC PATTERNS AT 200 AND 300 MILLIBARSSource: Journal of Meteorology:;1953:;volume( 010 ):;issue: 006::page 450Author:Teweles, Sidney
DOI: 10.1175/1520-0469(1953)010<0450:ATOTRB>2.0.CO;2Publisher: American Meteorological Society
Abstract: A proposed method of forecasting the occurrence of precipitation by forecasting the field of vorticity advection at 300 mb is tested in this study by verifying the concurrent relationship between the two phenomena. A similar verification is made of the relationship between precipitation and the field of 300-mb height-change advection and 200-mb temperature advection. Better verification is attained by means of the latter two patterns. The principal conclusion reached is that upper level charts do not contain sufficient information to permit accurate forecasting of precipitation without additional information from levels below 300 mb.
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contributor author | Teweles, Sidney | |
date accessioned | 2017-06-09T14:10:53Z | |
date available | 2017-06-09T14:10:53Z | |
date copyright | 1953/12/01 | |
date issued | 1953 | |
identifier issn | 0095-9634 | |
identifier other | ams-14033.pdf | |
identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4149550 | |
description abstract | A proposed method of forecasting the occurrence of precipitation by forecasting the field of vorticity advection at 300 mb is tested in this study by verifying the concurrent relationship between the two phenomena. A similar verification is made of the relationship between precipitation and the field of 300-mb height-change advection and 200-mb temperature advection. Better verification is attained by means of the latter two patterns. The principal conclusion reached is that upper level charts do not contain sufficient information to permit accurate forecasting of precipitation without additional information from levels below 300 mb. | |
publisher | American Meteorological Society | |
title | A TEST OF THE RELATION BETWEEN PRECIPITATION AND SYNOPTIC PATTERNS AT 200 AND 300 MILLIBARS | |
type | Journal Paper | |
journal volume | 10 | |
journal issue | 6 | |
journal title | Journal of Meteorology | |
identifier doi | 10.1175/1520-0469(1953)010<0450:ATOTRB>2.0.CO;2 | |
journal fristpage | 450 | |
journal lastpage | 456 | |
tree | Journal of Meteorology:;1953:;volume( 010 ):;issue: 006 | |
contenttype | Fulltext |