Overturning in the North Atlantic.

Published

Journal Article (Review)

The global overturning of ocean waters involves the equatorward transport of cold, deep waters and the poleward transport of warm, near-surface waters. Such movement creates a net poleward transport of heat that, in partnership with the atmosphere, establishes the global and regional climates. Although oceanographers have long assumed that a reduction in deep water formation at high latitudes in the North Atlantic translates into a slowing of the ocean's overturning and hence in Earth's climate, observational and modeling studies over the past decade have called this assumed linkage into question. The observational basis for linking water mass formation with the ocean's meridional overturning is reviewed herein. Understanding this linkage is crucial to efforts aimed at predicting the consequences of the warming and freshening of high-latitude surface waters to the climate system.

Full Text

Duke Authors

Cited Authors

  • Lozier, MS

Published Date

  • January 2012

Published In

Volume / Issue

  • 4 /

Start / End Page

  • 291 - 315

PubMed ID

  • 22457977

Pubmed Central ID

  • 22457977

Electronic International Standard Serial Number (EISSN)

  • 1941-0611

International Standard Serial Number (ISSN)

  • 1941-1405

Digital Object Identifier (DOI)

  • 10.1146/annurev-marine-120710-100740

Language

  • eng