i0091-7613-36-12-991.indd

ABSTRACT During the last deglaciation (ca. 21-10 ka), freshening of the North Atlantic surface likely caused reductions in Atlantic meridional overturning circulation (AMOC); the mechanisms related to AMOC recovery remain poorly understood. Here we present three new deglacial surface temperature and...

Full description

Bibliographic Details
Main Authors: Anders E Carlson, Delia W Oppo, Rosemarie E Came, †, Allegra N Legrande, Lloyd D Keigwin, William B Curry, Ericchristensen
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
North Atlantic
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1061.2037
http://geoscience.wisc.edu/geoscience/wp-content/uploads/2010/07/carlson_geology_2008_SSS.pdf
Description
Summary:ABSTRACT During the last deglaciation (ca. 21-10 ka), freshening of the North Atlantic surface likely caused reductions in Atlantic meridional overturning circulation (AMOC); the mechanisms related to AMOC recovery remain poorly understood. Here we present three new deglacial surface temperature and δ 18

Similar Items