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Helen Amanda Fricker Scripps Institution of Oceanography Ted Scambos National Snow and Ice Data Center Bob Bindschadler NASA/GSFC Space Flight Center Laurie.

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Presentation on theme: "Helen Amanda Fricker Scripps Institution of Oceanography Ted Scambos National Snow and Ice Data Center Bob Bindschadler NASA/GSFC Space Flight Center Laurie."— Presentation transcript:

1 Helen Amanda Fricker Scripps Institution of Oceanography Ted Scambos National Snow and Ice Data Center Bob Bindschadler NASA/GSFC Space Flight Center Laurie Padman Earth & Space Research Photos of Whillans Ice Stream courtesy of Lee Powell and Charlie Bentley, 1987-88 season & edited by Robert Phillips AAAS/NASA press briefing – San Francisco – 15 February 2007 Antarctic subglacial plumbing mapped from space

2 Helen Amanda Fricker Scripps Institution of Oceanography, La Jolla, CA AAAS/NASA press briefing – San Francisco – 15 February 2007

3 NASAs ICESat mission and launch Ice Cloud and land Elevation Satellite (ICESat) launched 12 Jan 2003 from Vandenberg, CA Primary goal of ICESat mission is ice sheet change detection AAAS/NASA press briefing – San Francisco – 15 February 2007

4 Schematic of single profile science data measurements, compiled through time to build elevation data sets ICESat laser altimeter Surface elevations along a ground track determined from laser time of flight, combined with precise orbit and pointing information ICESat has 3 lasers and is switched on for ~33 days every ~4 months in a repeat track pattern (which enabled this discovery) Geoscience Laser Altimeter System (GLAS) AAAS/NASA press briefing – San Francisco – 15 February 2007

5 ICESat repeat-track analysis + indicates surface uplift (filling) - indicates surface deflation (draining) ~ indicates oscillating (i.e. doing both) Conway Ridge Engelhardt Ridge Whillans Ice Stream (B) Mercer Ice Stream (A) Elevation range 2003-06 (m) 0 9m MOA (NSIDC) AAAS/NASA press briefing – San Francisco – 15 February 2007

6 Subglacial Lake Engelhardt Conway Ridge Engelhardt Ridge Largest event in magnitude: deflating WAIS Meeting 2006 ICESat elevation range (m) 09 Whillans Ice Stream (B) Mercer Ice Stream (A) AAAS/NASA press briefing – San Francisco – 15 February 2007

7 Ted Scambos National Snow and Ice Data Center, Boulder, CO (by telephone) AAAS/NASA press briefing – San Francisco – 15 February 2007

8 Conway Ridge Engelhardt Ridge Elevation range 2003-06 (m) 0 9m + indicates surface uplift (filling) - indicates surface deflation (draining) ~ indicates oscillating (i.e. doing both) Satellite image differencing Uplift Subsidence Whillans Ice Stream (B) Mercer Ice Stream (A) MOA (NSIDC) AAAS/NASA press briefing – San Francisco – 15 February 2007

9 Hydraulic potential map Conway Ridge Engelhardt Ridge Conway Ridge Engelhardt Ridge Whillans Ice Stream (B) Mercer Ice Stream (A) Whillans Ice Stream (B) Mercer Ice Stream (A) Elevation range 2003-06 (m) 0 9m MOA (NSIDC) AAAS/NASA press briefing – San Francisco – 15 February 2007

10 Hydraulic potential map Engelhardt Ridge Conway Ridge SGL Engelhardt SGL Conway SGL Whillans SGL Mercer IMPORTANT: This is *not* topography AAAS/NASA press briefing – San Francisco – 15 February 2007

11 MODIS difference image: December 2005 minus December 2002 Subglacial Lake Engelhardt AAAS/NASA press briefing – San Francisco – 15 February 2007

12 Bob Bindschadler NASA Goddard Space Flight Center, Greenbelt, MD AAAS/NASA press briefing – San Francisco – 15 February 2007

13 Drawdown vs time at 3 crossovers Subglacial Lake Engelhardt Total volume loss ~ 2.0 km 3 to ocean cavity under Ross Ice Shelf through subglacial channel AAAS/NASA press briefing – San Francisco – 15 February 2007

14 Conway Ridge Engelhardt Ridge Whillans Ice Stream (B) Mercer Ice Stream (A) How much water in the system? Isolated Subglacial Lake Engelhardt lost ~2.0 km 3 over the observation period (33 months) Elevation range 2003-06 (m) 0 9m -2.0 km 3 SgLE SgLC SgLM +1.2 km 3 +0.12 km 3 +0.27 km 3 SgLW Remainder of the system had a net gain ~1.6 km 3 over the same period (~0.6 km 3 a -1 ) Net water gain is likely both reflecting and influencing the motion of these major Antarctic ice sheet outlet streams AAAS/NASA press briefing – San Francisco – 15 February 2007


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