Constant wind regimes during the Last Glacial Maximum and early Holocene: Evidence from Little Llangothlin Lagoon, New England Tablelands, eastern Australia

Climate of the Past

Volumn 12, Issue 7, 2016, Pages 1435-1444

  Shulmeister, James ^a   Kemp, Justine ^b   Fitzsimmons, Kathryn E ^c   Gontz, Allen ^d,e  

^a UNIVERSITY OF QUEENSLAND   (Australia)

^b GRIFFITH UNIVERSITY   (Australia)

^c MAX PLANCK INSTITUTE FOR EVOLUTIONARY ANTHROPOLOGY   (Germany)

^d UNIVERSITY OF MASSACHUSETTS BOSTON   (United States)

^e SAN DIEGO STATE UNIVERSITY   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

ATMOSPHERIC CIRCULATION; BEACH; BERM; GEOMORPHOLOGY; GROUND PENETRATING RADAR; HOLOCENE; LAGOON; LAST GLACIAL MAXIMUM; LUMINESCENCE DATING; SOUTHERN HEMISPHERE; SUBTROPICAL REGION; WATER BUDGET; WESTERLY; WIND;

AUSTRALIA; NEW ENGLAND TABLELANDS; NEW SOUTH WALES;

EID: 84979681444     PISSN: 18149324     EISSN: 18149332     Source Type: Journal    
DOI: 10.5194/cp-12-1435-2016     Document Type: Article

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