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EOS, TRANSACTIONS AMERICAN GEOPHYSICAL UNION,
VOL. 88, NO. 13,
doi:10.1029/2007EO130001,
2007
Nearshore Arctic Subsea Permafrost in Transition
Volker Rachold
Research Department Potsdam, Alfred Wegener Institute, Potsdam, Germany International Arctic Science Committee, Stockholm
Dmitry Yu Bolshiyanov
Arctic and Antarctic Research Institute, St. Petersburg, Russia
Mikhail N. Grigoriev
Permafrost Institute, Siberian Branch of the Russian Academy of Sciences, Yakutsk, Russia
Hans-Wolfgang Hubberten
Research Department Potsdam, Alfred Wegener Institute, Potsdam, Germany
Ralf Junker
Institute of Geology, University of Bremen, Bremen, Germany
Victor V. Kunitsky
Permafrost Institute, Siberian Branch of the Russian Academy of Sciences, Yakutsk, Russia
Franziska Merker
Research Department Potsdam, Alfred Wegener Institute, Potsdam, Germany
Paul Overduin
Research Department Potsdam, Alfred Wegener Institute, Potsdam, Germany
Waldemar Schneider
Research Department Potsdam, Alfred Wegener Institute, Potsdam, Germany
Abstract
Models and geophysical data indicate that large areas of the Arctic shelves, as a result of their exposure during the Last
Glacial Maximum, are thought to be almost entirely underlain by subsea permafrost from the coastline down to a water depth
of about 100 meters. Subsea permafrost is still poorly understood, due mainly to the lack of direct observations. However,
it is known to contain gas hydrates, a solid phase composed of water and gases that formed under low-temperature, high-pressure
conditions. Large volumes of methane in gas hydrate form can be stored within or below the subsea permafrost, and the stability
of this gas hydrate zone is sustained by the existence of permafrost. Degradation of subsea permafrost and the consequent
destabilization of gas hydrates could significantly if not dramatically increase the flux of methane, a potent greenhouse
gas, to the atmosphere.
Published 27
March
2007.
Index Terms: 0702 Cryosphere: Permafrost (0475); 0772 Cryosphere: Distribution; 3002 Marine Geology and Geophysics: Continental shelf and slope processes (4219).
Print Version (273649 bytes)
Citation: Rachold, V., D. Y. Bolshiyanov, M. N. Grigoriev, H.-W. Hubberten, R. Junker, V. V. Kunitsky, F. Merker, P. Overduin, and W. Schneider
(2007),
Nearshore Arctic Subsea Permafrost in Transition,
Eos Trans. AGU,
88(13),
doi:10.1029/2007EO130001.
Copyright 2007 by the American Geophysical Union.
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