In:
Paleoceanography, American Geophysical Union (AGU), Vol. 32, No. 6 ( 2017-06), p. 622-633
Kurzfassung:
Precipitation over the Parnaíba watershed increased with decreasing AMOC during Heinrich stadial 1 The ITCZ location over northeastern Brazil changed in proportion to the Atlantic interhemispheric temperature gradient Off northeastern Brazil, the highest sediment discharge occurred during the transition from semiarid LGM to the wetter Heinrich stadial 1
Materialart:
Online-Ressource
ISSN:
0883-8305
,
1944-9186
DOI:
10.1002/2017PA003084
Sprache:
Englisch
Verlag:
American Geophysical Union (AGU)
Publikationsdatum:
2017
ZDB Id:
637876-6
ZDB Id:
2015231-0
ZDB Id:
2916554-4
SSG:
16,13
SSG:
13
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