. The Eastern Bering Sea Shelf : oceanography and resources / edited by Donald W. Hood and John A. Calder . 12:00 AM GMT 27 FEB 76 the passage of a low-pressure system crossing the usually no longer present, although some areas of Bering Sea. Southerly winds typically follow, how- unconsohdated pack-ice floes may be present, par- ever, facilitating the breakup and removal of the ticularly in the center of Norton Sound. At this time shorefast ice. By early June the shorefast ice is the distributary channels have been cleared of ice and

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