Detecting Holocene changes in thermohaline circulation
AUTOR(ES)
Keigwin, L. D.
FONTE
The National Academy of Sciences
RESUMO
Throughout the last glacial cycle, reorganizations of deep ocean water masses were coincident with rapid millennial-scale changes in climate. Climate changes have been less severe during the present interglacial, but evidence for concurrent deep ocean circulation change is ambiguous.
ACESSO AO ARTIGO
http://www.pubmedcentral.nih.gov/articlerender.fcgi?artid=34300Documentos Relacionados
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