Reconciling Bølling warmth with peak deglacial meltwater discharge

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 Green...

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Bibliographic Details
Main Authors: Lohmann, Gerrit, Schulz, Maximilian
Format: Article in Journal/Newspaper
Language:unknown
Published: 2000
Subjects:
Greenland
Greenland-Scotland Ridge
Online Access:https://epic.awi.de/id/eprint/11038/
https://hdl.handle.net/10013/epic.21498
id ftawi:oai:epic.awi.de:11038
record_format openpolar
spelling ftawi:oai:epic.awi.de:11038 2023-09-05T13:19:49+02:00 Reconciling Bølling warmth with peak deglacial meltwater discharge Lohmann, Gerrit Schulz, Maximilian 2000 https://epic.awi.de/id/eprint/11038/ https://hdl.handle.net/10013/epic.21498 unknown Lohmann, G. orcid:0000-0003-2089-733X and Schulz, M. (2000) Reconciling Bølling warmth with peak deglacial meltwater discharge , Paleoceanography, 15 (5), pp. 537-540 . hdl:10013/epic.21498 EPIC3Paleoceanography, 15(5), pp. 537-540 Article isiRev 2000 ftawi 2023-08-22T19:49:01Z 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. Article in Journal/Newspaper Greenland Greenland-Scotland Ridge Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) Greenland
institution Open Polar
collection Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center)
op_collection_id ftawi
language unknown
description 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.
format Article in Journal/Newspaper
author Lohmann, Gerrit
Schulz, Maximilian
spellingShingle Lohmann, Gerrit
Schulz, Maximilian
Reconciling Bølling warmth with peak deglacial meltwater discharge
author_facet Lohmann, Gerrit
Schulz, Maximilian
author_sort Lohmann, Gerrit
title Reconciling Bølling warmth with peak deglacial meltwater discharge
title_short Reconciling Bølling warmth with peak deglacial meltwater discharge
title_full Reconciling Bølling warmth with peak deglacial meltwater discharge
title_fullStr Reconciling Bølling warmth with peak deglacial meltwater discharge
title_full_unstemmed Reconciling Bølling warmth with peak deglacial meltwater discharge
title_sort reconciling bølling warmth with peak deglacial meltwater discharge
publishDate 2000
url https://epic.awi.de/id/eprint/11038/
https://hdl.handle.net/10013/epic.21498
geographic Greenland
geographic_facet Greenland
genre Greenland
Greenland-Scotland Ridge
genre_facet Greenland
Greenland-Scotland Ridge
op_source EPIC3Paleoceanography, 15(5), pp. 537-540
op_relation Lohmann, G. orcid:0000-0003-2089-733X and Schulz, M. (2000) Reconciling Bølling warmth with peak deglacial meltwater discharge , Paleoceanography, 15 (5), pp. 537-540 . hdl:10013/epic.21498
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