In:
Paleoceanography, American Geophysical Union (AGU), Vol. 30, No. 4 ( 2015-04), p. 353-368
Abstract:
AMOC still active during Heinrich Stadial 1 but weaker than during the LGM Weaker AMOC caused reduced NADW volume and NADW δ 13 C source decrease Amplitude of early deglacial δ 13 C decrease correlated to glacial NADW fraction
Type of Medium:
Online Resource
ISSN:
0883-8305
,
1944-9186
DOI:
10.1002/2014PA002667
Language:
English
Publisher:
American Geophysical Union (AGU)
Publication Date:
2015
detail.hit.zdb_id:
637876-6
detail.hit.zdb_id:
2015231-0
detail.hit.zdb_id:
2916554-4
SSG:
16,13
SSG:
13
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