Journal
JOURNAL OF GLACIOLOGY
Volume 64, Issue 243, Pages 1-11Publisher
CAMBRIDGE UNIV PRESS
DOI: 10.1017/jog.2017.73
Keywords
glacier flow; ice dynamics; ice velocity; remote sensing
Funding
- NASA MEaSUREs program (NASA) [NNX08AL98A, NNX13AI21A]
- NASA [NNX13AI21A, 473413, NNX08AL98A, 98200] Funding Source: Federal RePORTER
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While numerous maps of Greenland ice flow velocity exist, most have gaps in coverage and/or accuracy is limited. We processed a large volume of synthetic aperture radar and Landsat 8 imagery collected between 1995 and 2015 to produce a nearly complete map of ice flow velocity for Greenland at a far greater accuracy than most prior products. We evaluated the accuracy of this map by comparing it with a variety of measured and estimated velocities. For the slow-moving interior of the ice sheet, where estimates are determined from interferometric phase, the errors are similar to 2 m a(-1) or better. For coastal areas, where estimates are determined entirely from speckle-or feature-tracking methods, errors are 2-3 m a(-1), which is in good agreement with the estimated formal errors. Especially for the slow-moving majority of the ice sheet, this map provides an important source of data for numerous types of glaciological studies.
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