Author : Jerry A. Galt
Publisher :
Page : 56 pages
File Size : 38,62 MB
Release : 1975
Category : Hydrodynamics
ISBN :
[PDF] Development Of A Simplified Diagnostic Model For Interpretation Of Oceanographic Data eBook
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Development of a Simplified Diagnostic Model for Interpretation of Oceanographic Data
Author : Jerry A. Galt
Publisher :
Page : 46 pages
File Size : 11,17 MB
Release : 1975
Category : Hydrodynamics
ISBN :
Comprehensive Bibliography
Author : Outer Continental Shelf Environmental Assessment Program
Publisher :
Page : 632 pages
File Size : 47,75 MB
Release : 1984
Category : Continental shelf
ISBN :
Comprehensive Bibliography
Author :
Publisher :
Page : 764 pages
File Size : 19,32 MB
Release : 1988
Category : Continental shelf
ISBN :
CENFOR
Author : United States. Bureau of the Census
Publisher :
Page : 1326 pages
File Size : 50,71 MB
Release : 1971
Category : Electronic data processing
ISBN :
NOAA Professional Paper
Author :
Publisher :
Page : 324 pages
File Size : 49,30 MB
Release : 1979
Category : Atmosphere
ISBN :
Scientific and Technical Aerospace Reports
Author :
Publisher :
Page : 702 pages
File Size : 20,18 MB
Release : 1995
Category : Aeronautics
ISBN :
Monthly Catalog of United States Government Publications
Author :
Publisher :
Page : 1194 pages
File Size : 44,85 MB
Release : 1976
Category : Government publications
ISBN :
An Evaluation of Formulas for Estimating Clear-sky Insolation Over the Ocean
Author : Ronald K. Reed
Publisher :
Page : 874 pages
File Size : 25,15 MB
Release : 1975
Category : Atmospheric transparency
ISBN :
Recent oceanic data and observations from five coastal sites in the National Weather Service solar radiation network are compared with a formula for computing clear-sky insolation derived from the Smithsonian Meteorological Tables, using a transmission coefficient of 0.7. The results are generally in good agreement, and they suggest that this formula is suitable for computing insolation over the ocean for a wide range of latitudes. The comparison also indicates that a correction to the formula for middle latitudes is not warranted. The one other formula in good agreement with that form the Smithsonian Tables is one derived by Lumb; Laevastu's formula is only acceptable at sun angles less that 50°, and Berliands' estimates are too high at all solar altitudes. The formula from the Smithsonian Tables can be used to compute insolation over the oceans with a random error of estimate probably not exceeding 5% for periods of a few days or longer.
ESSA Professional Paper
Author : United States. National Oceanic and Atmospheric Administration
Publisher :
Page : 526 pages
File Size : 13,78 MB
Release : 1979
Category : Meteorology
ISBN :