Turbulent Atmospheric Parameters by Contaminant Deposition
Author: S. P. Zimmerman
Publisher:
Published: 1965
Total Pages: 18
ISBN-13:
DOWNLOAD EBOOKRead and Download eBook Full
Author: S. P. Zimmerman
Publisher:
Published: 1965
Total Pages: 18
ISBN-13:
DOWNLOAD EBOOKAuthor: S. P. Zimmerman
Publisher:
Published: 1966
Total Pages: 12
ISBN-13:
DOWNLOAD EBOOKAuthor: Andre? Sergeevich Monin
Publisher: Courier Corporation
Published: 2007-01-01
Total Pages: 898
ISBN-13: 0486458911
DOWNLOAD EBOOK"If ever a book on turbulence could be called definitive," declared Science, "it is this book by two of Russia's most eminent and productive scientists in turbulence, oceanography, and atmospheric physics." Noted for its clarity as well as its comprehensive treatment, this two-volume set serves as text or reference. 1975 edition.
Author:
Publisher:
Published: 1967
Total Pages: 686
ISBN-13:
DOWNLOAD EBOOKAuthor: Robert T. Dodd
Publisher:
Published: 1965
Total Pages: 20
ISBN-13:
DOWNLOAD EBOOKAuthor: Wayne S. Hering
Publisher:
Published: 1964
Total Pages: 280
ISBN-13:
DOWNLOAD EBOOKAuthor: John H. Conover
Publisher:
Published: 1965
Total Pages: 22
ISBN-13:
DOWNLOAD EBOOKAuthor: Gideon Kantor
Publisher:
Published: 1965
Total Pages: 36
ISBN-13:
DOWNLOAD EBOOKAuthor: Vernon G. Plank
Publisher:
Published: 1965
Total Pages: 214
ISBN-13:
DOWNLOAD EBOOKThe cumulus cloud events of the Florida peninsula that were observed during a 19-day period of photoreconnaissance in August and September 1957 are described and illustrated. The associated meteorological and rainfall events are also described and the intercorrelations among the various observations are pointed out. The study findings revealed that the principal factors governing the cloud and rainfall situations of the different days were (1) the low-level advection of water vapor into the peninsula from the oceanic surroundings, (2) the wind transport, into the heated peninsula from the oceans during the daytime, of pre -existing cumulus populations containing appreciable liquid water, (3) the low-level convergence, and associated updraft motion, engendered by the synoptic situation and the peninsula sea breezes, and (4) the precipitable water content of the lower Florida air mass. (Author)