Two millennia of tropical cyclone-induced mud layers in a northern Yucatán stalagmite: Multiple overlapping climatic hazards during the Maya Terminal Classic "megadroughts"

Geophysical Research Letters

Volumn 41, Issue 14, 2014, Pages 5148-5157

  Frappier, Amy Benoit ^a   Pyburn, James ^b   Pinkey Drobnis, Aurora D ^a   Wang, Xianfeng ^c   Corbett, D Reide ^d   Dahlin, Bruce H ^e  

^a SKIDMORE COLLEGE   (United States)

^b EXXONMOBIL UPSTREAM RESEARCH COMPANY   (United States)

^c NANYANG TECHNOLOGICAL UNIVERSITY   (Singapore)

^d EAST CAROLINA UNIVERSITY   (United States)

^e SHEPHERD UNIVERSITY   (United States)

Author keywords

Central America; drought; flood; Maya; paleoclimatology; proxy development

Indexed keywords

CAVES; DROUGHT; GEOCHRONOLOGY; HURRICANES; ISOTOPES;

CENTRAL AMERICA; MAYA; PALEOCLIMATOLOGY; PALEOTEMPESTOLOGY; PROXY DEVELOPMENT; RECURRENCE INTERVALS; TROPICAL CYCLONE; TWENTIETH CENTURY;

FLOODS;

CLIMATE CONDITIONS; CLIMATE VARIATION; DATING METHOD; DROUGHT; ESTIMATION METHOD; FLOODING; PALEOCLIMATE; STALAGMITE; TROPICAL CYCLONE; WATER TABLE;

YUCATAN PENINSULA;

EID: 84904843739     PISSN: 00948276     EISSN: 19448007     Source Type: Journal    
DOI: 10.1002/2014GL059882     Document Type: Article

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