Large-scale ocean circulation-cloud interactions reduce the pace of transient climate change

Geophysical Research Letters

Volumn 43, Issue 8, 2016, Pages 3935-3943

  Trossman, D S ^a,b,c   Palter, J B ^a,d   Merlis, T M ^a   Huang, Y ^a   Xia, Y ^a  

^a MCGILL UNIVERSITY   (Canada)

^b NASA GODDARD SPACE FLIGHT CENTER   (United States)

^c JOHNS HOPKINS UNIVERSITY   (United States)

^d UNIVERSITY OF RHODE ISLAND   (United States)

Author keywords

climate; clouds; feedbacks; MOC; ocean circulation; transient

Indexed keywords

ATMOSPHERIC MOVEMENTS; CARBON DIOXIDE; CLIMATE MODELS; CLOUDS; FEEDBACK; GLOBAL WARMING; OCEANOGRAPHY; TRANSIENTS;

ATMOSPHERIC MERIDIONAL HEAT TRANSPORT; CLIMATE; FEEDBACK MECHANISMS; LARGE-SCALE OCEAN CIRCULATIONS; OCEAN CIRCULATION; OCEANIC CIRCULATIONS; SPATIAL PATTERNS; TRANSIENT CLIMATE CHANGE;

CLIMATE CHANGE;

CARBON DIOXIDE; CLIMATE CHANGE; CLIMATE MODELING; CLOUD COVER; FEEDBACK MECHANISM; GLOBAL WARMING; OCEANIC CIRCULATION;

EID: 84968725152     PISSN: 00948276     EISSN: 19448007     Source Type: Journal    
DOI: 10.1002/2016GL067931     Document Type: Article

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