III.—On the Circulation of Salt in its Relations to Geology
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A Sea-Breeze is salt-laden in varying degree. On a fine dry day it may contain as much as 22 milligrams of salt per cubic metre of air (Armand Gautier, Bull. Soc. Chim., 1899 [iii], 21, 391–392). This invisible salt is washed out of the atmosphere by rains, and finds its way back to the sea.
1981 ◽
1981 ◽
2002 ◽
Vol 67
(553)
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pp. 37-41
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2002 ◽
Vol 29
(24)
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pp. 56-1-56-4
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1993 ◽
Vol 32
(1)
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pp. 116-125
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Meteorological observations of the coastal boundary layer structure at the Bulgarian Black Sea coast
2011 ◽
Vol 6
(1)
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pp. 251-259
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