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Fricker, HA, Powell R, Priscu J, Tulaczyk S, Anandakrishnan S, Christner B, Fisher AT, Holland D, Horgan H, Jacobel R, Mikucki J, Mitchell A, Scherer R, Severinghaus J.  2011.  Siple Coast subglacial aquatic environments; the Whillans ice stream subglacial access research drilling project. Geophysical Monograph. 192:199-219.   10.1029/2010gm000932   AbstractWebsite

The Whillians Ice Stream Subglacial Access Research Drilling (WISSARD) project is a 6-year (2009-2015) integrative study of ice sheet stability and subglacial geobiology in West Antarctica, funded by the Antarctic Integrated System Science Program of National Science Foundation's Office of Polar Programs, Antarctic Division. The overarching scientific objective of WISSARD is to assess the role of water beneath a West Antarctic Ice Stream in interlinked glaciological, geological, microbiological, geochemical, hydrological, and oceanographic systems. The WISSARD's important science questions relate to (1) the role that subglacial and ice shelf cavity waters and wet sediments play in ice stream dynamics and mass balance, with an eye on the possible future of the West Antarctic Ice Sheet and (2) the microbial metabolic and phylogenetic diversity in these subglacial environments. The study area is the downstream part of the Whillans Ice Stream on the Siple Coast, specifically Subglacial Lake Whillans and the part of the grounding zone across which it drains. In this chapter, we provide background on the motivation for the WISSARD project, detail the key scientific goals, and describe the new measurement tools and strategies under development that will provide the framework for conducting an unprecedented range of scientific observations.

Aciego, SM, Cuffey KM, Kavanaugh JL, Morse DL, Severinghaus JP.  2007.  Pleistocene ice and paleo-strain rates at Taylor Glacier, Antarctica. Quaternary Research. 68:303-313.   10.1016/j.yqres.2007.07.013   AbstractWebsite

Ice exposed in ablation zones of ice sheets can be a valuable source of samples for paleoclimate studies and information about long-term ice dynamics. We report a 28-km long stable isotope sampling transect along a flowline on lower Taylor Glacier, Antarctica, and show that ice from the last glacial period is exposed here over tens of kilometers. Gas isotope analyses on a small number of samples confirm our age hypothesis. These chronostratigraphic data contain information about past ice dynamics and in particular should be sensitive to the longitudinal strain rate on the north flank of Taylor Dome, averaged over millennia. The imprint of climatic changes on ice dynamics may be discernible in these data. (c) 2007 University of Washington. All rights reserved.

Taylor, KC, White JWC, Severinghaus JP, Brook EJ, Mayewski PA, Alley RB, Steig EJ, Spencer MK, Meyerson E, Meese DA, Lamorey GW, Grachev A, Gow AJ, Barnett BA.  2004.  Abrupt climate change around 22 ka on the Siple Coast of Antarctica. Quaternary Science Reviews. 23:7-15.   10.1016/j.quascirev.2003.09.004   AbstractWebsite

A new ice core from Siple Dome, Antarctica suggests the surface temperature increased by similar to6degreesC in just several decades at approximately 22 ka BP. This abrupt change did not occur 500 kin away in the Byrd ice core, or in climate proxy records in the Siple Dome core indicative of the mid-latitude Pacific. This demonstrates there was significant spatial heterogeneity in the response of the Antarctic climate during the last deglaciation and draws attention to unexplained mechanisms of abrupt climate change in Antarctica. (C) 2003 Elsevier Ltd. All rights reserved.