. The Eastern Bering Sea Shelf : oceanography and resources / edited by Donald W. Hood and John A. Calder. Oceanography Bering SEASONAL PACK ICE STAMUKHI ZONE -SHOREFAST ICE- Floating fast Bottomfast ice ' ice. Yrr^rrrrrrrT^^-^TTrr^' ,i;frr^^'^^'^- e^ "> of sub-ice channel) Sea pack ice. Pack ice rarely enters the sound from Norton Sound is relatively complex. In general the the west except during prolonged periods of strong ice flows mainly to the south in response to the westerly winds. prevailing northerly winds. Significant reversals in The pattern of ice movement to the west
. The Eastern Bering Sea Shelf : oceanography and resources / edited by Donald W. Hood and John A. Calder. Oceanography Bering SEASONAL PACK ICE STAMUKHI ZONE -SHOREFAST ICE- Floating fast Bottomfast ice ' ice. Yrr^rrrrrrrT^^-^TTrr^' ,i;frr^^'^^'^- e^ "> of sub-ice channel) Sea pack ice. Pack ice rarely enters the sound from Norton Sound is relatively complex. In general the the west except during prolonged periods of strong ice flows mainly to the south in response to the westerly winds. prevailing northerly winds. Significant reversals in The pattern of ice movement to the west of the path of the flow can occur, however, as illustrated. 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 Hood, D. W. (Donald Wilbur), 1918-; Calder, John A; United States. Office of Marine Pollution Assessment; United States. Bureau of Land Management. [Rockville, Md. ?] : U. S. Dept. of Commerce, National Oceanic and Atmospheric Administration, Office of Marine Pollution Assessment ; Seattle, Wash. : Distributed by the University of Washington Press
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Keywords: ., bookcentury1900, bookcollectionamericana, bookdecade1980, bookspo
