. The Andes of southern Peru; geographical reconnaissance along the seventy-third meridian. Yale Peruvian Expedition (1911); Physical geography; Geology. CLIMATOLOGY OF THE PERUVIAN ANDES 129 curve b. Hence, unusual atmospheric disturbances would result in heavier and more frequent showers. Turning now to local factors we find on the west coast a re- gional topography that favors a diurnal periodicity of air move- ment. The strong slopes of the Cordillera and the Coast Kange create up-slope or eastward air gradients by day and opposite , 1893-'95 2 Please note that these images
. The Andes of southern Peru; geographical reconnaissance along the seventy-third meridian. Yale Peruvian Expedition (1911); Physical geography; Geology. CLIMATOLOGY OF THE PERUVIAN ANDES 129 curve b. Hence, unusual atmospheric disturbances would result in heavier and more frequent showers. Turning now to local factors we find on the west coast a re- gional topography that favors a diurnal periodicity of air move- ment. The strong slopes of the Cordillera and the Coast Kange create up-slope or eastward air gradients by day and opposite , 1893-'95 2 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 Bowman, Isaiah, 1878-1950; American Geographical Society of New York. New York, Published for the Americsn Geographical Society of New York by H. Holt
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Keywords: ., bookauthorbo, bookcentury1900, bookdecade1910, booksubjectgeology
