Sea-level rise in Southwest Greenland as a contributor to Viking abandonment

The first records of Greenland Vikings date to 985 CE. Archaeological evidence yields insight into how Vikings lived, yet drivers of their disappearance in the 15th century remain enigmatic. Research suggests a combination of environmental and socioeconomic factors, and the climatic shift from the M...

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Published in:Proceedings of the National Academy of Sciences
Main Authors: Borreggine, Marisa, Latychev, Konstantin, Coulson, Sophie Leanne, Powell, Evelyn M., Mitrovica, Jerry X., Milne, Glenn A., Alley, Richard B.
Language:unknown
Published: 2023
Subjects:
Online Access:http://www.osti.gov/servlets/purl/1972987
https://www.osti.gov/biblio/1972987
https://doi.org/10.1073/pnas.2209615120
id ftosti:oai:osti.gov:1972987
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spelling ftosti:oai:osti.gov:1972987 2023-07-30T04:03:41+02:00 Sea-level rise in Southwest Greenland as a contributor to Viking abandonment Borreggine, Marisa Latychev, Konstantin Coulson, Sophie Leanne Powell, Evelyn M. Mitrovica, Jerry X. Milne, Glenn A. Alley, Richard B. 2023-07-10 application/pdf http://www.osti.gov/servlets/purl/1972987 https://www.osti.gov/biblio/1972987 https://doi.org/10.1073/pnas.2209615120 unknown http://www.osti.gov/servlets/purl/1972987 https://www.osti.gov/biblio/1972987 https://doi.org/10.1073/pnas.2209615120 doi:10.1073/pnas.2209615120 54 ENVIRONMENTAL SCIENCES 2023 ftosti https://doi.org/10.1073/pnas.2209615120 2023-07-11T10:26:58Z The first records of Greenland Vikings date to 985 CE. Archaeological evidence yields insight into how Vikings lived, yet drivers of their disappearance in the 15th century remain enigmatic. Research suggests a combination of environmental and socioeconomic factors, and the climatic shift from the Medieval Warm Period (~900 to 1250 CE) to the Little Ice Age (~1250 to 1900 CE) may have forced them to abandon Greenland. Glacial geomorphology and paleoclimate research suggest that the Southern Greenland Ice Sheet readvanced during Viking occupation, peaking in the Little Ice Age. Counterintuitively, the readvance caused sea-level rise near the ice margin due to increased gravitational attraction toward the ice sheet and crustal subsidence. We estimate ice growth in Southwestern Greenland using geomorphological indicators and lake core data from previous literature. We calculate the effect of ice growth on regional sea level by applying our ice history to a geophysical model of sea level with a resolution of ~1 km across Southwestern Greenland and compare the results to archaeological evidence. The results indicate that sea level rose up to ~3.3 m outside the glaciation zone during Viking settlement, producing shoreline retreat of hundreds of meters. Sea-level rise was progressive and encompassed the entire Eastern Settlement. Moreover, pervasive flooding would have forced abandonment of many coastal sites. These processes likely contributed to the suite of vulnerabilities that led to Viking abandonment of Greenland. Sea-level change thus represents an integral, missing element of the Viking story. Other/Unknown Material Greenland Greenland Sea Ice Sheet SciTec Connect (Office of Scientific and Technical Information - OSTI, U.S. Department of Energy) Greenland Proceedings of the National Academy of Sciences 120 17
institution Open Polar
collection SciTec Connect (Office of Scientific and Technical Information - OSTI, U.S. Department of Energy)
op_collection_id ftosti
language unknown
topic 54 ENVIRONMENTAL SCIENCES
spellingShingle 54 ENVIRONMENTAL SCIENCES
Borreggine, Marisa
Latychev, Konstantin
Coulson, Sophie Leanne
Powell, Evelyn M.
Mitrovica, Jerry X.
Milne, Glenn A.
Alley, Richard B.
Sea-level rise in Southwest Greenland as a contributor to Viking abandonment
topic_facet 54 ENVIRONMENTAL SCIENCES
description The first records of Greenland Vikings date to 985 CE. Archaeological evidence yields insight into how Vikings lived, yet drivers of their disappearance in the 15th century remain enigmatic. Research suggests a combination of environmental and socioeconomic factors, and the climatic shift from the Medieval Warm Period (~900 to 1250 CE) to the Little Ice Age (~1250 to 1900 CE) may have forced them to abandon Greenland. Glacial geomorphology and paleoclimate research suggest that the Southern Greenland Ice Sheet readvanced during Viking occupation, peaking in the Little Ice Age. Counterintuitively, the readvance caused sea-level rise near the ice margin due to increased gravitational attraction toward the ice sheet and crustal subsidence. We estimate ice growth in Southwestern Greenland using geomorphological indicators and lake core data from previous literature. We calculate the effect of ice growth on regional sea level by applying our ice history to a geophysical model of sea level with a resolution of ~1 km across Southwestern Greenland and compare the results to archaeological evidence. The results indicate that sea level rose up to ~3.3 m outside the glaciation zone during Viking settlement, producing shoreline retreat of hundreds of meters. Sea-level rise was progressive and encompassed the entire Eastern Settlement. Moreover, pervasive flooding would have forced abandonment of many coastal sites. These processes likely contributed to the suite of vulnerabilities that led to Viking abandonment of Greenland. Sea-level change thus represents an integral, missing element of the Viking story.
author Borreggine, Marisa
Latychev, Konstantin
Coulson, Sophie Leanne
Powell, Evelyn M.
Mitrovica, Jerry X.
Milne, Glenn A.
Alley, Richard B.
author_facet Borreggine, Marisa
Latychev, Konstantin
Coulson, Sophie Leanne
Powell, Evelyn M.
Mitrovica, Jerry X.
Milne, Glenn A.
Alley, Richard B.
author_sort Borreggine, Marisa
title Sea-level rise in Southwest Greenland as a contributor to Viking abandonment
title_short Sea-level rise in Southwest Greenland as a contributor to Viking abandonment
title_full Sea-level rise in Southwest Greenland as a contributor to Viking abandonment
title_fullStr Sea-level rise in Southwest Greenland as a contributor to Viking abandonment
title_full_unstemmed Sea-level rise in Southwest Greenland as a contributor to Viking abandonment
title_sort sea-level rise in southwest greenland as a contributor to viking abandonment
publishDate 2023
url http://www.osti.gov/servlets/purl/1972987
https://www.osti.gov/biblio/1972987
https://doi.org/10.1073/pnas.2209615120
geographic Greenland
geographic_facet Greenland
genre Greenland
Greenland Sea
Ice Sheet
genre_facet Greenland
Greenland Sea
Ice Sheet
op_relation http://www.osti.gov/servlets/purl/1972987
https://www.osti.gov/biblio/1972987
https://doi.org/10.1073/pnas.2209615120
doi:10.1073/pnas.2209615120
op_doi https://doi.org/10.1073/pnas.2209615120
container_title Proceedings of the National Academy of Sciences
container_volume 120
container_issue 17
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