Synthesizing multiple remote-sensing techniques for subglacial hydrologic mapping: application to a lake system beneath MacAyeal Ice Stream, West Antarctica

Abstract We present an analysis of the active hydrologic system of MacAyeal Ice Stream (MacIS), West Antarctica, from a synthesis of multiple remote-sensing techniques: satellite laser altimetry; satellite image differencing; and hydrologic potential mapping (using a satellite-derived DEM and a bedrock DEM from airborne radio-echo sounding). Combining these techniques augments the information provided by each one individually, and allows us to develop a protocol for studying subglacial hydrologic systems in a holistic manner. Our study reveals five large active subglacial lakes under MacIS, the largest of which undergoes volume changes of at least 1.0 km3. We discuss the hydrologic properties of this system and present evidence for links between the lakes. At least three of the lakes are co-located with sticky spots, i.e. regions of high local basal shear stress. We also find evidence for surface elevation changes due to ice-dynamic effects (not just water movement) caused by changes in basal resistance. Lastly, we show that satellite radar altimetry is of limited use for monitoring lake activity on fast-flowing ice streams with surfaces that undulate on ∼10 km length scales.

[1]  D. Drewry Radio echo sounding map of Antarctica, (˜90°E–180°) , 1975, Polar Record.

[2]  R. Armstrong,et al.  The Physics of Glaciers , 1981 .

[3]  Observed Velocity Fluctuations on a Major Antarctic Ice Stream , 1989 .

[4]  H Engelhardt,et al.  Physical Conditions at the Base of a Fast Moving Antarctic Ice Stream , 1990, Science.

[5]  R. Bindschadler,et al.  Satellite-Image-Derived Velocity Field of an Antarctic Ice Stream , 1991, Science.

[6]  D. Macayeal The basal stress distribution of Ice Stream E, Antarctica, inferred by control methods , 1992 .

[7]  Improved resolution ice sheet mapping with satellite radar altimeters , 1993 .

[8]  W. Cudlip,et al.  IDENTIFICATION OF SUBGLACIAL LAKES USING ERS-1 RADAR ALTIMETER , 1993 .

[9]  P. L. Vornberger,et al.  Detailed elevation map of Ice Stream C, Antarctica, using satellite imagery and airborne radar , 1994 .

[10]  M. Siegert,et al.  A large deep freshwater lake beneath the ice of central East Antarctica , 1996, Nature.

[11]  Breaking the seal at Grímsvötn, Iceland , 1999 .

[12]  David G. Vaughan,et al.  BEDMAP: a new ice thickness and subglacial topographic model of Antarctica , 2001 .

[13]  Theodore A. Scambos,et al.  An image-enhanced DEM of the Greenland ice sheet , 2002, Annals of Glaciology.

[14]  D. Roy,et al.  Achieving sub-pixel geolocation accuracy in support of MODIS land science , 2002 .

[15]  Ian Joughin,et al.  Basal shear stress of the Ross ice streams from control method inversions , 2004 .

[16]  Kenneth C. Jezek,et al.  Evidence for subglacial water transport in the West Antarctic Ice Sheet through three‐dimensional satellite radar interferometry , 2004 .

[17]  S. Carter,et al.  A revised inventory of Antarctic subglacial lakes , 2004, Antarctic Science.

[18]  H. Fricker,et al.  Ice shelf grounding zone structure from ICESat laser altimetry , 2006 .

[19]  Yonghong Li,et al.  Improved Methods for Analysis of Decadal Elevation-Change Time Series Over Antarctica , 2006, IEEE Transactions on Geoscience and Remote Sensing.

[20]  C. Clark,et al.  Subglacial floods beneath ice sheets , 2006, Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences.

[21]  Duncan J. Wingham,et al.  Rapid discharge connects Antarctic subglacial lakes , 2006, Nature.

[22]  Chris D. Clark,et al.  Ice stream sticky spots: A review of their identification and influence beneath contemporary and palaeo-ice streams , 2007 .

[23]  Helen Amanda Fricker,et al.  An Active Subglacial Water System in West Antarctica Mapped from Space , 2007, Science.

[24]  T. Painter,et al.  MODIS-based Mosaic of Antarctica (MOA) data sets: Continent-wide surface morphology and snow grain size , 2007 .

[25]  D. Macayeal,et al.  Causes of sudden, short‐term changes in ice‐stream surface elevation , 2007 .

[26]  T. Scambos,et al.  Enhancing a RADARSAT/ICESat Digital Elevation Model of West Antarctica Using MODIS Imagery , 2007 .

[27]  Leigh A. Stearns,et al.  Increased flow speed on a large East Antarctic outlet glacier caused by subglacial floods , 2008 .

[28]  Jonathan L. Bamber,et al.  A new 1 km Digital Elevation Model of the Antarctic Derived From Combined Satellite Radar and Laser Data , 2008 .

[29]  M. E. Peters,et al.  Dynamic distributed drainage implied by the flow evolution of the 1996–1998 Adventure Trench subglacial lake discharge , 2009 .

[30]  Mònica Roca,et al.  The EnviSat RA-2 Instrument Design and Tracking Performance , 2009, IEEE Transactions on Geoscience and Remote Sensing.

[31]  B. Smith,et al.  An inventory of active subglacial lakes in Antarctica detected by ICESat (2003–2008) , 2009, Journal of Glaciology.

[32]  Helen Amanda Fricker,et al.  Connected subglacial lake activity on lower Mercer and Whillans Ice Streams, West Antarctica, 2003–2008 , 2009, Journal of Glaciology.

[33]  R. Alley,et al.  Seismic observations of transient subglacial water‐flow beneath MacAyeal Ice Stream, West Antarctica , 2009 .

[34]  Kelly M. Brunt,et al.  Mapping the grounding zone of the Ross Ice Shelf, Antarctica, using ICESat laser altimetry , 2010, Annals of Glaciology.

[35]  R. Bindschadler,et al.  Ice Sheet Change Detection by Satellite Image Differencing , 2010 .

[36]  D. Macayeal,et al.  Basal friction of Ice Stream E, West Antarctica , 1995, Journal of Glaciology.