hdl:10013/epic.21498

Reconciling Bølling warmth with peak deglacial meltwater discharge


Lohmann, Gerrit ORCID: https://orcid.org/0000-0003-2089-733X and Schulz, Maximilian ;
Contact
lohmann [ at ] awi-bremerhaven.de

Abstract

Paleoclimatic data indicate warm conditions during the Bølling period, whereas climate modeling studies predict significant cooling, triggered by the concomitant deglacial meltwater flux into the Atlantic Ocean. We suggest that the lack of an adequate representation of deep-water flow over the Greenland-Scotland Ridge in ocean circulation models can account for this discrepancy.



Item Type
Article
Authors
Lohmann, Gerrit ORCID: https://orcid.org/0000-0003-2089-733X and Schulz, Maximilian ;
Divisions
Non-AWI items
Programs
Basic Research > Helmholtz Independent Research
Publication Status
Published
Eprint ID
11038
Cite as
Lohmann, G. and Schulz, M. (2000): Reconciling Bølling warmth with peak deglacial meltwater discharge , Paleoceanography, 15 (5), pp. 537-540 .


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