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Acknowledgments: We thank the NIH (grant GM-55382) and
the U.S. Department of Energy (grant DE-FG02-07ER15843)
for financial support and the Univ. of Illinois and the
American Chemical Society Division of Organic Chemistry
(sponsored by Boehringer Ingelheim) for fellowship
support (D.W.R.). We also thank P. Hergenrother
(Univ. of Illinois), M. Burke (Univ. of Illinois), and
S. Herzon (Yale Univ.) for helpful discussions.
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Supporting Online Material
Materials and Methods
SOM Text
Figs. S1 to S5
Table S1
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28. Intermolecular hydroamination of an alkyne has been
reported with complexes of Group IV metals that are
air-sensitive and generally suffer from poor functional-group
compatibility, and it has been catalyzed by complexes of
the precious metals palladium, rhodium, and gold.
References (46–50)
4 May 2011; accepted 6 July 2011
10.1126/science.1207922
tures (1). Until now, however, the vast extent of
East Antarctica, which comprises 77% of the
continent, has been devoid of quality data; only
a few floating ice shelves have been mapped,
and comprehensive velocity mapping has been
limited to the lower reaches of key outlet gla-
ciers (2).
Balance velocity calculated from ice thick-
ness, surface slope, and snow accumulation data
provides insights about the potential flow pat-
tern of the ice sheet (3), but the technique as-
sumes an ice sheet in mass equilibrium, which
is not correct everywhere, and that ice flows
perpendicular to surface contours, which is a
Ice Flow of the Antarctic Ice Sheet
E. Rignot,1,2* J. Mouginot,1 B. Scheuchl1
We present a reference, comprehensive, high-resolution, digital mosaic of ice motion in Antarctica
assembled from multiple satellite interferometric synthetic-aperture radar data acquired during
the International Polar Year 2007 to 2009. The data reveal widespread, patterned, enhanced
flow with tributary glaciers reaching hundreds to thousands of kilometers inland over the entire
continent. This view of ice sheet motion emphasizes the importance of basal-slip–dominated
tributary flow over deformation-dominated ice sheet flow, redefines our understanding of ice
sheet dynamics, and has far-reaching implications for the reconstruction and prediction of ice
sheet evolution.
ce velocity is a fundamental characteristic of ground-based stations are limited relative to the
glaciers and ice sheets that measures the rate size of the continent, leading to an incomplete
at which ice is transported from the interior picture of Antarctica. Satellite radar interferom-
1Department of Earth System Science, University of California
Irvine, Irvine, CA 92697, USA. 2Jet Propulsion Laboratory, Cal-
ifornia Institute of Technology, Pasadena, CA 91109, USA.
I
regions toward the ocean, the location of pre- etry, or InSAR, has been successfully used to
ferred channels of ice transport, and how ice mass map glacier flow independent of cloud cover,
evolves with time. Traditional measurements from solar illumination, or the presence of surface fea- erignot@uci.edu
*To whom correspondence should be addressed. E-mail:
1427