. Compendium of meteorology. Meteorology. - 80 >â eo 2 40 20 L 6 S G S C G C G C L 1420 0400 1430. Pig. LâRegistrations of wind speed and direction, temperature, and relative humidity during the characteristic land- and sea-breeze days from June 3 to June 5, 1932, at Danzig (L = land breeze, S = sea breeze, G = gradient wind, C = calm). {After Koschmieder [54].) As an example of the tropical form of the land and sea breezes the diagram of velocity isopleths by van Bemmelen of the land and sea breezes at Batavia is reproduced in Fig. 3. It is also an example of the vertical velocity distribu


. Compendium of meteorology. Meteorology. - 80 >â eo 2 40 20 L 6 S G S C G C G C L 1420 0400 1430. Pig. LâRegistrations of wind speed and direction, temperature, and relative humidity during the characteristic land- and sea-breeze days from June 3 to June 5, 1932, at Danzig (L = land breeze, S = sea breeze, G = gradient wind, C = calm). {After Koschmieder [54].) As an example of the tropical form of the land and sea breezes the diagram of velocity isopleths by van Bemmelen of the land and sea breezes at Batavia is reproduced in Fig. 3. It is also an example of the vertical velocity distribution during the course of a day. Explanation of the Land and Sea Breezes. The cause of the land and sea breezes must undoubtedly be 1300. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original American Meteorological Society. Committee on the Compendium of Meteorology; Malone, Thomas F. Boston : American Meteorological Society


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