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Title: Glacial terminations and the global water budget

Technical Report ·
OSTI ID:5831217
 [1]
  1. Columbia Univ., Palisades, NY (United States). Lamont-Doherty Geological Observatory

Evidence suggests that the last glacial period came to an abrupt close about 13,500 years ago. This evidence indicates: (1) that the melting of the North American ice sheet commenced abruptly at this time; (2) that surface temperatures in the northern Atlantic rose sharply at this time; (3) that surface water conditions in the Antarctic changed abruptly at this time; (4) that the salinity of the Red Sea dropped abruptly at this time; and (5) that accumulation rate of planktonic foraminifera in the South China Sea underwent an abrupt five-fold increase at this time. This project has been directed toward better developing and documenting our explanation for the abruptness of these changes. This project has supported investigation of several aspects of this hypothesis. We suggest that the Greenland climate changes are driven by oscillations in salt content which modulate the strength of the Atlantic's conveyor circulation.

Research Organization:
Lawrence Livermore National Lab., CA (United States); Columbia Univ., Palisades, NY (United States). Lamont-Doherty Geological Observatory
Sponsoring Organization:
USDOE; USDOE, Washington, DC (United States)
DOE Contract Number:
W-7405-ENG-48
OSTI ID:
5831217
Report Number(s):
UCRL-CR-109709; ON: DE92008939
Country of Publication:
United States
Language:
English