Articles | Volume 18, issue 3
https://doi.org/10.5194/tc-18-1399-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/tc-18-1399-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
27 Mar 2024
Research article |
| 27 Mar 2024
| 27 Mar 2024
Sea-ice variations and trends during the Common Era in the Atlantic sector of the Arctic Ocean
Ana Lúcia Lindroth Dauner
CORRESPONDING AUTHOR
Environmental Change Research Unit (ECRU), Ecosystems and Environment Research Programme, Faculty of Biological and Environmental Sciences, University of Helsinki, Helsinki, 00014, Finland
Department of Geosciences and Geography, University of Helsinki, Helsinki, 00014, Finland
Frederik Schenk
Department of Geosciences and Geography, University of Helsinki, Helsinki, 00014, Finland
Bolin Centre for Climate Research, Stockholm University, Stockholm, 10691, Sweden
Department of Geological Sciences, Stockholm University, Stockholm, 10691, Sweden
Katherine Elizabeth Power
Bolin Centre for Climate Research, Stockholm University, Stockholm, 10691, Sweden
Department of Physical Geography, Stockholm University, Stockholm, 10691, Sweden
Maija Heikkilä
Environmental Change Research Unit (ECRU), Ecosystems and Environment Research Programme, Faculty of Biological and Environmental Sciences, University of Helsinki, Helsinki, 00014, Finland
Helsinki Institute of Sustainability Science (HELSUS), University of Helsinki, Helsinki, 00014, Finland
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Using climate model simulations, we find that SE Asian tropical climate was strongly seasonal under Late Glacial conditions. During Northern Hemisphere winters, it was highly arid in this region that is today humid year-round. The seasonal aridity was driven by orbital forcing and stronger East Asian winter monsoon. A breakdown of deep convection caused a reorganized Walker Circulation and a mean state resembling El Niño conditions.
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Short summary
In this study, we analysed 14 sea-ice proxy records and compared them with the results from two different climate simulations from the Atlantic sector of the Arctic Ocean over the Common Era (last 2000 years). Both proxy and model approaches demonstrated a long-term sea-ice increase. The good correspondence suggests that the state-of-the-art sea-ice proxies are able to capture large-scale climate drivers. Short-term variability, however, was less coherent due to local-to-regional scale forcings.
In this study, we analysed 14 sea-ice proxy records and compared them with the results from two...
