An Evaluation of Formulas for Estimating Clear-sky Insolation Over the Ocean

An Evaluation of Formulas for Estimating Clear-sky Insolation Over the Ocean PDF Author: Ronald K. Reed
Publisher:
ISBN:
Category : Atmospheric transparency
Languages : en
Pages : 874

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Book Description
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.

An Evaluation of Formulas for Estimating Clear-sky Insolation Over the Ocean

An Evaluation of Formulas for Estimating Clear-sky Insolation Over the Ocean PDF Author: Ronald K. Reed
Publisher:
ISBN:
Category : Atmospheric transparency
Languages : en
Pages : 874

Get Book Here

Book Description
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.

Monthly Catalog of United States Government Publications

Monthly Catalog of United States Government Publications PDF Author:
Publisher:
ISBN:
Category : Government publications
Languages : en
Pages : 1194

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An Evaluation of Cloud Factors for Estimating Insolation Over the Ocean

An Evaluation of Cloud Factors for Estimating Insolation Over the Ocean PDF Author: Ronald K. Reed
Publisher:
ISBN:
Category : Clouds
Languages : en
Pages : 34

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Solar Radiation Over India

Solar Radiation Over India PDF Author: Anna Mani and S. Rangarajan
Publisher: Allied Publishers
ISBN:
Category :
Languages : en
Pages : 662

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Business Service Check List PDF Author:
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Category : Industries
Languages : en
Pages : 8

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ISBN:
Category : Aeronautics
Languages : en
Pages : 1034

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ISBN:
Category :
Languages : en
Pages : 732

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Category : Electronic journals
Languages : en
Pages : 1110

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Publisher:
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Category :
Languages : en
Pages : 36

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United States Department of Commerce Publications, Catalog and Index

United States Department of Commerce Publications, Catalog and Index PDF Author: United States. Department of Commerce. Library
Publisher:
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Category : United States
Languages : en
Pages : 92

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