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A new velocity map for Byrd Glacier, East Antarctica, from sequential ASTER satellite imagery

机译:来自南极东部的伯德冰川的新速度图,来自连续的ASTER卫星图像

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New ice-velocity measurements are obtained for the main trunk of Byrd Glacier, East Antarctica, using recently acquired Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) imagery. The velocities are derived from the application of a cross-correlation technique to sequential images acquired in 2000 and 2001. Images were co-registered and ortho-rectified with the aid of a digital elevation model (DEM) generated from ASTER stereo imagery. This paper outlines the process of DEM generation, image co-registration and correction, and the application of the cross-correlation technique to obtain ice velocities. Comparison of the new velocity map with earlier measurements of velocity from 1978 indicates that the glacier has undergone a substantial deceleration between observations. Portions of the glacier flowing at speeds of ~850 m a?1 in 1978/79 were flowing at ~650 m a?1 in 2000/01. The cause of this change in ice dynamics is not known, but the observation shows that East Antarctic outlet glaciers can undergo substantial changes on relat ively short timescales.
机译:使用最近获得的先进星载热发射和反射辐射计(ASTER)图像,可以获取东南极伯德冰川主干的新冰速测量结果。速度是通过对2000年和2001年获取的连续图像应用互相关技术得出的。图像相互配准,并借助从ASTER立体图像生成的数字高程模型(DEM)进行正射校正。本文概述了DEM的生成,图像共配准和校正的过程,以及互相关技术在获得冰速度方面的应用。新的速度图与1978年以来的早期速度测量值的比较表明,冰川在两次观测之间经历了实质性的减速。在1978/79年,部分冰川以〜850 m a?1的速度流动,在2000/01年以650 m a?1的速度流动。冰动力学变化的原因尚不清楚,但观察结果表明,南极东部出口冰川可能在相对较短的时间尺度上发生实质性变化。

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