In:
Paleoceanography and Paleoclimatology, American Geophysical Union (AGU), Vol. 34, No. 7 ( 2019-07), p. 1107-1123
Kurzfassung:
The Western Pacific Warm Pool was warmer in the early Holocene and cooled toward the present because of changes in insolation‐driven tropical Pacific mean state The Holocene cooling was mostly felt in the southern Indo‐Pacific Warm Pool regions likely responding to a complex combination of climatic processes The deglacial Indo‐Pacific Warm Pool temperatures raised gradually similar to the atmospheric CO 2 and/or Antarctica temperature changes
Materialart:
Online-Ressource
ISSN:
2572-4517
,
2572-4525
DOI:
10.1029/2018PA003455
Sprache:
Englisch
Verlag:
American Geophysical Union (AGU)
Publikationsdatum:
2019
ZDB Id:
2916554-4