Sheltering coefficient: Difference between revisions

From Glossary of Meteorology
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|Meaning=The constant of proportionality in Jeffreys's expression for the [[work]] done  by the [[wind]] on the sea surface.
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|Explanation=It was assumed by Jeffreys that this work is proportional to the product of the [[density]] of air,  the slope of the water surface, and the square of the wind velocity relative to the [[wave]]. Although  the value of the sheltering coefficient (0.27) found by Jeffreys gives a satisfactory explanation of  the initial formation of [[wind waves]], observations of the increase of wind waves shows that this  value is about ten times too high for the subsequent [[transfer]] of [[energy]] from wind to waves.
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== sheltering coefficient ==
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<div class="definition"><div class="short_definition">The constant of proportionality in Jeffreys's expression for the [[work]] done  by the [[wind]] on the sea surface.</div><br/> <div class="paragraph">It was assumed by Jeffreys that this work is proportional to the product of the [[density]] of air,  the slope of the water surface, and the square of the wind velocity relative to the [[wave]]. Although  the value of the sheltering coefficient (0.27) found by Jeffreys gives a satisfactory explanation of  the initial formation of [[wind waves]], observations of the increase of wind waves shows that this  value is about ten times too high for the subsequent [[transfer]] of [[energy]] from wind to waves.</div><br/> </div>
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Latest revision as of 05:25, 30 March 2024

The constant of proportionality in Jeffreys's expression for the work done by the wind on the sea surface.

It was assumed by Jeffreys that this work is proportional to the product of the density of air, the slope of the water surface, and the square of the wind velocity relative to the wave. Although the value of the sheltering coefficient (0.27) found by Jeffreys gives a satisfactory explanation of the initial formation of wind waves, observations of the increase of wind waves shows that this value is about ten times too high for the subsequent transfer of energy from wind to waves.

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