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Member Since 2014
Christof Pearce
Associate Professor, Aarhus University
AGU Research
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Climate Variability and Glacier Dynamics Linked to Fjord Productivity Changes Over the Last ca. 3300 Years in Nuup Kangerlua, Southwest Greenland
PALEOCEANOGRAPHY AND PALEOCLIMATOLOGY
29 february 2024
Mimmi Oksman, Anna Bang, Christof Pearce, Niels J....
Greenlandic fjords, located between the ice sheet and the ocean, are dynamic systems that can sustain highly variable levels of primary productivit...
Seasonal Sea Ice in the Arctic’s Last Ice Area during the Early Holocene
PAST CLIMATE CHANGE IN EARTH'S POLAR REGIONS: LESSONS FOR THE FUTURE II POSTER
paleoceanography and paleoclimatology | 16 december 2022
Henrieka Detlef, Matt O'Regan, Christian Stranne, ...
The northern coastline of Greenland, comprising the Lincoln Sea, is a unique sea ice regime. It is part of the Arctic Oceans last ice area, suggested ...
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A Dynamic Holocene North Greenland Ice Sheet: The Marine Sediment Perspective
HOW STABLE IS THE GREENLAND ICE SHEET? PAST, PRESENT, AND FUTURE I ORAL
cryosphere | 16 december 2022
Brendan T. Reilly, Anne E. Jennings, Matt O'Regan,...
North Greenland is home to the few remaining floating marine termini of the Greenland Ice Sheet (GIS), including the Petermann and Ryder Ice Tongues. ...
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Deglaciation and Holocene paleoceanography of the northeast Greenland Shelf
HOW STABLE IS THE GREENLAND ICE SHEET? PAST, PRESENT, AND FUTURE II POSTER
cryosphere | 16 december 2022
Christof Pearce, Katrine J. Andresen, Joanna Davie...
The broad continental shelf offshore northeast Greenland features large trough systems and glacial landforms indicating the presence of fast flowing i...
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Late Holocene Paleomagnetic Secular Variation in the Chukchi Sea, Arctic Ocean
GEOCHEMISTRY, GEOPHYSICS, GEOSYSTEMS
09 may 2022
Gabriel West, Andreas Nilsson, Alexis Geels, Marti...
The geomagnetic field behavior in polar regions remains poorly understood and documented. Although a number of Late Holocene paleomagnetic secular ...
Holocene sea ice dynamics in Petermann Fjord - implications for the stability of Petermann ice tongue
A WARMING ARCTIC: WHAT RECORDS OF THE PAST TELL US ABOUT THE FUTURE III POSTERS
paleoceanography and paleoclimatology | 12 december 2019
Henrieka Detlef, Brendan T. Reilly, Anne E. Jennin...
Marine-terminating outlet glaciers play a fundamental role in the mass loss of the Greenland ice sheet due to non-linear behavior promoted by ice-ocea...
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Holocene paleoceanographic development of the eastern Baffin Bay
A WARMING ARCTIC: WHAT RECORDS OF THE PAST TELL US ABOUT THE FUTURE III POSTERS
paleoceanography and paleoclimatology | 12 december 2019
Katrine E. Elnegaard Hansen, Jacques Giraudeau, A...
The 738 cm long marine sediment core (core AMD14-204C; 73°15.663 N/57°53.987 W; 987 m water depth) provides a Holocene paleoceanographic and paleoclim...
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New marine reservoir age corrections from coastal Greenland waters and the eastern Arctic Ocean
ADVANCES IN AGE MODEL DEVELOPMENTS FOR PALEOCEANOGRAPHY AND PALEOCLIMATOLOGY I POSTERS
paleoceanography and paleoclimatology | 10 december 2019
Christof Pearce, Jesper Olsen, Matt O'Regan, Marti...
Radiocarbon (14C) dating is the standard method for obtaining the age of marine sediments of Holocene and late Pleistocene age. For accurate calibrati...
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