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首页> 外文期刊>Journal of Glaciology >A complete map of Greenland ice velocity derived from satellite data collected over 20 years
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A complete map of Greenland ice velocity derived from satellite data collected over 20 years

机译:从20年超过20年的卫星数据得分的格陵兰冰速度完整地图

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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.
机译:虽然存在许多格陵兰冰流速的地图,但大多数都有覆盖范围和/或精度的差距。 我们在1995年至2015年间收集了大量的合成孔径雷达和Landsat 8图像,以生产比大多数现有产品更高的精度更高的格陵兰冰流速地图。 我们通过将其与各种测量和估计的速度进行比较来评估该地图的准确性。 对于冰盖的缓慢移动内部,其中从干涉阶段确定估计,误差类似于2m A(-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,错误是2-3米(-1),这与估计的正式错误吻合良好。 特别是对于大多数冰盖的慢速移动,该地图提供了许多类型的冰川学研究的重要数据来源。

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