This award is funded under the American Recovery and Reinvestment Act of 2009 (Public Law 111-5). The West Antarctic Ice Sheet is believed to be vulnerable to climate change as it is grounded below sea level, is drained by rapidly flowing ice streams and is fringed by floating ice shelves subject to melting by incursions of relatively warm Antarctic circumpolar water. Currently, the most rapidly thinning glaciers in Antarctica occur in the Amundsen and Bellingshausen Sea sectors. This study seeks to place the present day observations into a longer-term geological context over a broad scale by high-resolution swath bathymetric mapping of continental shelf sea floor features that indicate past ice presence and behavior. Gaps in existing survey coverage of glacial lineations and troughs indicating ice flow direction and paleo-grounding zone wedges over the Ross, Amundsen and Bellingshausen Sea sectors are targeted. The surveys will be conducted as part of the 2010 Icebreaker Oden science opportunity and will take advantage of the vessel's state-of-the-art swath mapping system.
N: -70.9 S: -74.75 E: -101.0 W: -108.0
|Temporal Extent:||Platform(s):||R/V NBP, SHIPS|
Title: Paleo ice flow and subglacial meltwater dynamics in Pine Island Bay, West Antarctica
Publication Date: 2013-01-01
Author(s): Nitsche, F.O., Gohl, K., Larter, R.D., Hillenbrand, C.D., Kuhn, G., Smith, J.A., Jacobs, S., Anderson, J.B., Jakobsson, M.
Series: The Cryosphere
Online Resource: Not provided
|Resolution||Range Begin||Range End||Unit of Measure||Accuracy|
|Project Short Name||Campaigns||Project Dates|
|NSF/PLR||No campaigns listed.||No dates provided.|
|Coverage Type||Zone Identifier||Geometry||Granule Representation|
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