. Bulletin. Science; Natural history; Natural history. \»-^14 2„j/'^IO 22 23,0^ \;. 15 16 X^14 11 ^^13 14 "^2 IJi?,.!"/^'^ ^-^'^^il NOV 15 3^ o 10 16 23 5 ^U DEC 2 6 MPH smh Fig. 3. Resultant Winds: La Habra. from those recorded al the other sites. Hence, the land and sea breeze tlow stiuc- tiire will differ from the more coastal locations. The first aspect of the surface air flow at Habra examined is the land breeze (Fig. 3). The greatest duration, as one might expect, occurs during the winter. Please note that these images are extracted from scanned page images that may have be
. Bulletin. Science; Natural history; Natural history. \»-^14 2„j/'^IO 22 23,0^ \;. 15 16 X^14 11 ^^13 14 "^2 IJi?,.!"/^'^ ^-^'^^il NOV 15 3^ o 10 16 23 5 ^U DEC 2 6 MPH smh Fig. 3. Resultant Winds: La Habra. from those recorded al the other sites. Hence, the land and sea breeze tlow stiuc- tiire will differ from the more coastal locations. The first aspect of the surface air flow at Habra examined is the land breeze (Fig. 3). The greatest duration, as one might expect, occurs during the winter. 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 Southern California Academy of Sciences. Los Angeles, Calif. : The Academy
Size: 2179px × 1147px
Photo credit: © Library Book Collection / Alamy / Afripics
License: Licensed
Model Released: No
Keywords: ., bookcentury1900, booksubjectnaturalhistory, booksubjectscience
