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...

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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
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.1061.2037 2023-05-15T17:28:40+02:00 i0091-7613-36-12-991.indd Anders E Carlson Delia W Oppo Rosemarie E Came † Allegra N Legrande Lloyd D Keigwin William B Curry Ericchristensen The Pennsylvania State University CiteSeerX Archives application/pdf 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 en eng 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 Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://geoscience.wisc.edu/geoscience/wp-content/uploads/2010/07/carlson_geology_2008_SSS.pdf text ftciteseerx 2020-04-19T00:19:36Z 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 Text North Atlantic Unknown
institution Open Polar
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op_collection_id ftciteseerx
language English
description 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
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author Anders E Carlson
Delia W Oppo
Rosemarie E Came
†
Allegra N Legrande
Lloyd D Keigwin
William B Curry
Ericchristensen
spellingShingle Anders E Carlson
Delia W Oppo
Rosemarie E Came
†
Allegra N Legrande
Lloyd D Keigwin
William B Curry
Ericchristensen
i0091-7613-36-12-991.indd
author_facet Anders E Carlson
Delia W Oppo
Rosemarie E Came
†
Allegra N Legrande
Lloyd D Keigwin
William B Curry
Ericchristensen
author_sort Anders E Carlson
title i0091-7613-36-12-991.indd
title_short i0091-7613-36-12-991.indd
title_full i0091-7613-36-12-991.indd
title_fullStr i0091-7613-36-12-991.indd
title_full_unstemmed i0091-7613-36-12-991.indd
title_sort i0091-7613-36-12-991.indd
url 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
genre North Atlantic
genre_facet North Atlantic
op_source http://geoscience.wisc.edu/geoscience/wp-content/uploads/2010/07/carlson_geology_2008_SSS.pdf
op_relation 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
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
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