. Compendium of meteorology. Meteorology. OBSERVATIONS AND THEORY OP MICROSEISMS 1305 gation of the microseismic waves in the ground to the energy of these waves is transferred to the coast; / de- point of observation. pends on the steepness of the coast, the loss of energy Energy Transmitted from Surf. The energy trans- due to friction in the water approaching the coast, and mitted from surf to the coast [14] depends on the the wind. The kinetic energy E* (per second) of ocean. Please note that these images are extracted from scanned page images that may have been digitally enhanced for reada
. Compendium of meteorology. Meteorology. OBSERVATIONS AND THEORY OP MICROSEISMS 1305 gation of the microseismic waves in the ground to the energy of these waves is transferred to the coast; / de- point of observation. pends on the steepness of the coast, the loss of energy Energy Transmitted from Surf. The energy trans- due to friction in the water approaching the coast, and mitted from surf to the coast [14] depends on the the wind. The kinetic energy E* (per second) of ocean. 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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Keywords: ., bookcentury1900, bookcollectionbiodivers, booksubjectmeteorology
