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contributor authorSchulz, Teresa M.
contributor authorSamson, Perry J.
date accessioned2017-06-09T14:02:16Z
date available2017-06-09T14:02:16Z
date copyright1988/04/01
date issued1988
identifier issn0894-8763
identifier otherams-11321.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4146537
description abstractNonprecipitating low cloud frequencies for 1982 have been extracted from the U.S. Air Force 3-Dimensional Nephanalysis archives for central North America. These data were compiled from satellite, surface and pilot reports and contain, among other parameters, the low cloud type and present weather code for each 3-h time period for grid points in the Northern Hemisphere. The overall average precipitating to nonprecipitating low cloud ratio for central North America was 0.25, indicating that nonpredpitating low clouds were very common. Seasonal frequencies of these nonprecipitating low clouds are presented. The persistence of clear and nonprecipitating cloudy skies from one time period to the next was also calculated on a seasonal basis. Annual average values for transitions between clear and cloudy skies as well as between nonprecipitating and precipitating low cloudy time periods are also presented. A cluster analysis was performed on the seasonal nonprecipitating low cloud frequency data. It was found that the original 4096 grid points could be described well by seven robust clusters. Thew clusters are identified and their distinguishing characteristics are discussed. It was found that not only were these clusters distinct from one another, but they exhibited considerable within-cluster consistency.
publisherAmerican Meteorological Society
titleNonprecipitating Low Cloud Frequencies for Central North America: 1982
typeJournal Paper
journal volume27
journal issue4
journal titleJournal of Applied Meteorology
identifier doi10.1175/1520-0450(1988)027<0427:NLCFFC>2.0.CO;2
journal fristpage427
journal lastpage440
treeJournal of Applied Meteorology:;1988:;volume( 027 ):;issue: 004
contenttypeFulltext


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