A Complete Map of Greenland Ice Velocity Derived from Satellite Data Collected over 20 Years.

IF 2.6
The journal of glaciology Pub Date : 2018-02-01 Epub Date: 2017-11-21 DOI:10.1017/jog.2017.73
Ian Joughin, Ben E Smith, Ian M Howat
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Abstract

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 (SAR) 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 ~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.

Abstract Image

Abstract Image

Abstract Image

根据20年来收集的卫星数据绘制的格陵兰冰速度完整地图。
虽然格陵兰岛冰流速度的地图很多,但大多数地图的覆盖范围和/或准确性有限。我们处理了1995年至2015年间收集的大量合成孔径雷达(SAR)和陆地卫星8号图像,以比大多数以前的产品更高的精度绘制了一张几乎完整的格陵兰冰流速度图。我们通过将这张地图与各种测量和估计的速度进行比较来评估其准确性。对于缓慢移动的冰盖内部,根据干涉相位确定估计值,误差约为2ma-1或更好。对于沿海地区,估计完全由散斑或特征跟踪方法确定,误差为2-3m-1,这与估计的形式误差非常一致。特别是对于缓慢移动的大部分冰盖,这张地图为许多类型的冰川学研究提供了重要的数据来源。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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