Climate change threatens archaeologically significant ice patches: insights into their age, internal structure, mass balance and climate sensitivity

Despite numerous spectacular archaeological discoveries worldwide related to melting ice patches and the emerging field of glacial archaeology, governing processes related to ice patch development during the Holocene and their sensitivity to climate change are still largely unexplored. Here we prese...

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Main Authors: R. S. Ødegård, A. Nesje, K. Isaksen, L. M. Andreassen, T. Eiken, M. Schwikowski, C. Uglietti
Format: Article
Language:English
Published: Copernicus Publications 2017-01-01
Series:The Cryosphere
Online Access:http://www.the-cryosphere.net/11/17/2017/tc-11-17-2017.pdf
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author R. S. Ødegård
A. Nesje
K. Isaksen
L. M. Andreassen
T. Eiken
M. Schwikowski
C. Uglietti
author_facet R. S. Ødegård
A. Nesje
K. Isaksen
L. M. Andreassen
T. Eiken
M. Schwikowski
C. Uglietti
author_sort R. S. Ødegård
collection DOAJ
description Despite numerous spectacular archaeological discoveries worldwide related to melting ice patches and the emerging field of glacial archaeology, governing processes related to ice patch development during the Holocene and their sensitivity to climate change are still largely unexplored. Here we present new results from an extensive 6-year (2009–2015) field experiment at the Juvfonne ice patch in Jotunheimen in central southern Norway. Our results show that the ice patch has existed continuously since the late Mesolithic period. Organic-rich layers and carbonaceous aerosols embedded in clear ice show ages spanning from modern at the surface to ca. 7600 cal years BP at the bottom. This is the oldest dating of ice in mainland Norway. The expanding ice patch covered moss mats appearing along the margin of Juvfonne about 2000 years ago. During the study period, the mass balance record showed a strong negative balance, and the annual balance is highly asymmetric over short distances. Snow accumulation is poorly correlated with estimated winter precipitation, and single storm events may contribute significantly to the total winter balance. Snow accumulation is approx. 20 % higher in the frontal area compared to the upper central part of the ice patch. There is sufficient meltwater to bring the permeable snowpack to an isothermal state within a few weeks in early summer. Below the seasonal snowpack, ice temperatures are between −2 and −4 °C. Juvfonne has clear ice stratification of isochronic origin.
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spelling doaj.art-a65dc4d6e25442069fafbfe813dd0d7b2022-12-22T00:12:42ZengCopernicus PublicationsThe Cryosphere1994-04161994-04242017-01-01111173210.5194/tc-11-17-2017Climate change threatens archaeologically significant ice patches: insights into their age, internal structure, mass balance and climate sensitivityR. S. Ødegård0A. Nesje1K. Isaksen2L. M. Andreassen3T. Eiken4M. Schwikowski5C. Uglietti6Norwegian University of Science and Technology, Gjøvik, NorwayUniversity of Bergen, Bergen, NorwayNorwegian Meteorological Institute, Oslo, NorwayNorwegian Water Resources and Energy Directorate, Oslo, NorwayDepartment of Geosciences, University of Oslo, Oslo, NorwayPaul Scherrer Institute, Villigen, SwitzerlandPaul Scherrer Institute, Villigen, SwitzerlandDespite numerous spectacular archaeological discoveries worldwide related to melting ice patches and the emerging field of glacial archaeology, governing processes related to ice patch development during the Holocene and their sensitivity to climate change are still largely unexplored. Here we present new results from an extensive 6-year (2009–2015) field experiment at the Juvfonne ice patch in Jotunheimen in central southern Norway. Our results show that the ice patch has existed continuously since the late Mesolithic period. Organic-rich layers and carbonaceous aerosols embedded in clear ice show ages spanning from modern at the surface to ca. 7600 cal years BP at the bottom. This is the oldest dating of ice in mainland Norway. The expanding ice patch covered moss mats appearing along the margin of Juvfonne about 2000 years ago. During the study period, the mass balance record showed a strong negative balance, and the annual balance is highly asymmetric over short distances. Snow accumulation is poorly correlated with estimated winter precipitation, and single storm events may contribute significantly to the total winter balance. Snow accumulation is approx. 20 % higher in the frontal area compared to the upper central part of the ice patch. There is sufficient meltwater to bring the permeable snowpack to an isothermal state within a few weeks in early summer. Below the seasonal snowpack, ice temperatures are between −2 and −4 °C. Juvfonne has clear ice stratification of isochronic origin.http://www.the-cryosphere.net/11/17/2017/tc-11-17-2017.pdf
spellingShingle R. S. Ødegård
A. Nesje
K. Isaksen
L. M. Andreassen
T. Eiken
M. Schwikowski
C. Uglietti
Climate change threatens archaeologically significant ice patches: insights into their age, internal structure, mass balance and climate sensitivity
The Cryosphere
title Climate change threatens archaeologically significant ice patches: insights into their age, internal structure, mass balance and climate sensitivity
title_full Climate change threatens archaeologically significant ice patches: insights into their age, internal structure, mass balance and climate sensitivity
title_fullStr Climate change threatens archaeologically significant ice patches: insights into their age, internal structure, mass balance and climate sensitivity
title_full_unstemmed Climate change threatens archaeologically significant ice patches: insights into their age, internal structure, mass balance and climate sensitivity
title_short Climate change threatens archaeologically significant ice patches: insights into their age, internal structure, mass balance and climate sensitivity
title_sort climate change threatens archaeologically significant ice patches insights into their age internal structure mass balance and climate sensitivity
url http://www.the-cryosphere.net/11/17/2017/tc-11-17-2017.pdf
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