High-resolution analyses of an early Holocene climate event may imply decreased solar forcing as an important climate trigger

Geology

Volumn 29, Issue 12, 2001, Pages 1107-1110

  Bjorck S ^a   Muscheler, R ^a   Kromer, B ^a   Andresen, C S ^a   Heinemeier, J ^a   Johnsen, S J ^a   Conley, D ^a   Koc N ^a   Spurk, M ^a   Veski, S ^a  

^a LUND UNIVERSITY   (Sweden)

Author keywords

14C; 10Be; 14C modeling; Holocene; Ice core proxies; Lake sediments; Marine records; Solar forcing; Sub Milankovitch cooling event; Tree rings

Indexed keywords

FRESHWATER FORCINGS;

CLIMATE CHANGE; COOLING; ICE; VENTILATION;

GEOLOGY;

BERYLLIUM; CLIMATE FORCING; COOLING; HOLOCENE; NORTHERN HEMISPHERE; PALEOCLIMATE; SOLAR ACTIVITY; THERMOHALINE CIRCULATION;

EID: 84879889091     PISSN: 00917613     EISSN: None     Source Type: Journal    
DOI: 10.1130/0091-7613(2001)029<1107:HRAOAE>2.0.CO;2     Document Type: Article

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