At that time, observations were lacking in the remote Amundsen Sea, where difficult ice conditions have vexed explorers for more than 200 years. Maksym, T., S.E. Oceanic heat transport onto the Amundsen Sea shelf through a submarine glacial trough. Fast recession of a West Antarctic glacier. Joughin, I., and R.B. 2012. Schodlok, M.P., D. Menemenlis, E. Rignot, and M. Studinger.
A model study of circulation and cross-shelf exchange on the west Antarctic Peninsula continental shelf. Heimbach, P., and M. Losch. Dowdeswell, and J. Evans. Pp.
Antarctica with the location of the Amundsen Sea. Inland thinning of the Amundsen Sea sector, West Antarctica.
1998.
Lake amundsenhavet (Norwegian: amundsenhavet) is a marginal sea of the south polar sea ... to the Bellingshausen Lake, immediately west of the Siple island to the Wrigley golf and 1000 kilometers further to the west lies the Ross Sea. Pp. Related to Geologic TimeGeomagnetism Graham, K. Gohl, G. Kuhn, C.-D. Hillenbrand, J.A. Glacially scoured troughs in the seafloor provide conduits for that seawater to melt regional ice shelves far more rapidly near their deep grounding lines.
Jenkins, A., P. Dutrieux, S. Jacobs, S. McPhail, J. Perrett, A. Webb, and D. White.
Meredith, Z. Wang, and A. Orr. Smedsrud, and K.M. Amundsen Sea Sea; Roald Amundsen Norwegian explorer; Wiki Authority Control Authority control is a method of creating and maintaining index terms for bibliographical material in a library catalogue. Dalziel, I.W.D., D.V. 2011. Antarctic ice sheet melting in the Southeast Pacific. Stability of the West Antarctic ice sheet in a warming world. Thomas, R.H. 1979. Variability of basal melt beneath the Pine Island Glacier ice shelf, West Antarctica. 2011. Red areas show the coverage of the multibeam bathymetry data, blue lines represent tracks of individual soundings, and green areas represent additional data sets that we used for areas covered by continental ice. Circulation and melting beneath George VI Ice Shelf, Antarctica. 2002. 238
Nitsche, F.O., S.S. Jacobs, R. Larter and K. Gohl. The Amundsen Sea continental shelf is one of the most remote areas of coastal Antarctica and was relatively unexplored until the late 1980s. Water characteristics of the Southern Ocean south of the Polar Front. Mapping of its ocean structure and circulation began in 1994, revealing that “warm” Circumpolar Deep Water has access to its continental shelf.
Caspian sea is located between Asia and Europe. This new compilation is a major improvement over previously available regional maps and should aid the numerical modeling of ocean circulation, the reconstructions of paleo‐ice streams, and the refinement of ice sheet models.The Amundsen Sea continental shelf is located between 100° and 135°W, south of 71°S, along the margin of the Marie Byrd Land sector of the West Antarctic Ice Sheet (WAIS) (Much of the rapid melting occurs within deep troughs on the inner shelf, presumably cut when the ice streams of larger ice sheets were grounded on the present seafloor [While several previous studies of Amundsen Sea bathymetry provided significant new insights, most have been restricted to local areas covered by single cruises. Autonomous underwater vehicle exploration of the ocean cavity beneath an Antarctic ice shelf. Holland, A.P. A model of tidally dominated ocean processes near ice shelf grounding lines.
Pp.
Concerns about their sensitivity to climate change were centered on air temperature and on glacially paced ice dynamics. Seaward of the coastline, the continental shelf narrows westward from >400 km north of Pine Island Bay to 100–200 km west of Siple Island. At that time, observations were lacking in the remote Amundsen Sea, where difficult ice conditions have vexed explorers for more than 200 years.
Oceanographic observations at the shelf break of the Amundsen Sea, Antarctica. Doake, A. Jenkins, and D.G. Quantification of ice shelf basal melting using a global finite-element sea ice-ice shelf-ocean model. Carmack, E.C. Hellmer, and H.J.R.
Concerns about their sensitivity to climate change were centered on air temperature and on glacially paced ice dynamics. Sixty-four days of hydrography and storms: RVIB Thoma, M., A. Jenkins, D. Holland, and S. Jacobs. 15–41 in Chavanne, C.P., K.J. Gordon, A.L.
2012. Pp. Mishinov. Similarly, models of the ocean circulation must properly account for this remarkable continental shelf, its fringing ice shelves and persistent sea ice cover. Transport and water masses of the Antarctic Slope Front system in the eastern Weddell Sea.