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Lagged atmospheric circulation response in the Black Sea region to Greenland Interstadial 10

Czymzik, Markus LU ; Nowaczyk, Norbert R. ; Dellwig, Olaf ; Wegwerth, Antje ; Muscheler, Raimund LU orcid ; Christl, Marcus and Arz, Helge W. (2020) In Proceedings of the National Academy of Sciences of the United States of America 117(46). p.28649-28654
Abstract

Northern Hemispheric high-latitude climate variations during the last glacial are expected to propagate globally in a complex way. Investigating the evolution of these variations requires a precise synchronization of the considered environmental archives. Aligning the globally common production rate variations of the cosmogenic radionuclide 10Be in different archives provides a tool for such synchronizations. Here, we present a 10Be record at <40-y resolution along with subdecadal proxy records from one Black Sea sediment core around Greenland Interstadial 10 (GI-10) ∼41 ka BP and the Laschamp geomagnetic excursion. We synchronized our 10Be record to that from Greenland ice cores based on its globally common production rate... (More)

Northern Hemispheric high-latitude climate variations during the last glacial are expected to propagate globally in a complex way. Investigating the evolution of these variations requires a precise synchronization of the considered environmental archives. Aligning the globally common production rate variations of the cosmogenic radionuclide 10Be in different archives provides a tool for such synchronizations. Here, we present a 10Be record at <40-y resolution along with subdecadal proxy records from one Black Sea sediment core around Greenland Interstadial 10 (GI-10) ∼41 ka BP and the Laschamp geomagnetic excursion. We synchronized our 10Be record to that from Greenland ice cores based on its globally common production rate variations. The synchronized environmental proxy records reveal a bipartite climate response in the Black Sea region at the onset of GI-10. First, in phase with Greenland warming, reduced sedimentary coastal ice rafted detritus contents indicate less severe winters. Second, and with a lag of 190 (± 44) y, an increase in the detrital K/Ti ratio and authigenic Ca precipitation point to enhanced regional precipitation and warmer lake surface temperatures. We explain the lagged climatic response by a shift in the dominant mode of atmospheric circulation, likely connected with a time-transgressive adjustment of the regional thermal ocean interior to interstadial conditions.

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author
; ; ; ; ; and
organization
publishing date
type
Contribution to journal
publication status
published
subject
keywords
archive synchronization, Black Sea sediments, climate, cosmogenic radionuclides, phase relationship
in
Proceedings of the National Academy of Sciences of the United States of America
volume
117
issue
46
pages
6 pages
publisher
National Academy of Sciences
external identifiers
  • pmid:33139546
  • scopus:85096359623
ISSN
1091-6490
DOI
10.1073/pnas.2005520117
language
English
LU publication?
yes
id
fbbe6382-dc30-46ea-8ecd-9f1fcff2b6f9
date added to LUP
2020-11-30 14:11:14
date last changed
2024-06-13 02:10:50
@article{fbbe6382-dc30-46ea-8ecd-9f1fcff2b6f9,
  abstract     = {{<p>Northern Hemispheric high-latitude climate variations during the last glacial are expected to propagate globally in a complex way. Investigating the evolution of these variations requires a precise synchronization of the considered environmental archives. Aligning the globally common production rate variations of the cosmogenic radionuclide 10Be in different archives provides a tool for such synchronizations. Here, we present a 10Be record at &lt;40-y resolution along with subdecadal proxy records from one Black Sea sediment core around Greenland Interstadial 10 (GI-10) ∼41 ka BP and the Laschamp geomagnetic excursion. We synchronized our 10Be record to that from Greenland ice cores based on its globally common production rate variations. The synchronized environmental proxy records reveal a bipartite climate response in the Black Sea region at the onset of GI-10. First, in phase with Greenland warming, reduced sedimentary coastal ice rafted detritus contents indicate less severe winters. Second, and with a lag of 190 (± 44) y, an increase in the detrital K/Ti ratio and authigenic Ca precipitation point to enhanced regional precipitation and warmer lake surface temperatures. We explain the lagged climatic response by a shift in the dominant mode of atmospheric circulation, likely connected with a time-transgressive adjustment of the regional thermal ocean interior to interstadial conditions.</p>}},
  author       = {{Czymzik, Markus and Nowaczyk, Norbert R. and Dellwig, Olaf and Wegwerth, Antje and Muscheler, Raimund and Christl, Marcus and Arz, Helge W.}},
  issn         = {{1091-6490}},
  keywords     = {{archive synchronization; Black Sea sediments; climate; cosmogenic radionuclides; phase relationship}},
  language     = {{eng}},
  number       = {{46}},
  pages        = {{28649--28654}},
  publisher    = {{National Academy of Sciences}},
  series       = {{Proceedings of the National Academy of Sciences of the United States of America}},
  title        = {{Lagged atmospheric circulation response in the Black Sea region to Greenland Interstadial 10}},
  url          = {{http://dx.doi.org/10.1073/pnas.2005520117}},
  doi          = {{10.1073/pnas.2005520117}},
  volume       = {{117}},
  year         = {{2020}},
}