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Surface configuration of the Antarctic ice sheet in the sector 30゜E - 80゜E using SEASAT altimetry data

机译:使用sEasaT测高数据在30°E-80°E的扇区中对南极冰盖的表面构造

摘要

Using Interim Geophysical Data Record (IGDR) of SEASAT radar altimetry, a configuration map of the Antarctic ice sheet in the area bounded by 30°and 80°E and latitude 72°S is compiled. A total of 7480 footprint data of every second sampling (6.62km apart) along 63 subsatellite groundtracks are obtained in the area. The area was divided into rectangles with side lengths of 0.1°in latitude and 0.4°in longitude, and the average elevation above sea level by SEASAT altimetry data within the rectangle is used for computer-aided contouring. Since the height error for 147 crossover points on the ice sheet was±6.7m in standard deviation, and height errors from slope-induced effect and other sources were 20m, the contour interval of 100m was chosen for an inland area higher than 500m above sea level. The obtained configuration resembles the map published by the Scott Polar Research Institute (1983). A total of 157 ground survey data from triangulation survey, satellite Doppler positioning and previously published topographic map are used to estimate an overall accuracy of the obtained configuration map. The ground survey height is on an average 2.2m lower than the SEASAT-derived elevation with a standard deviation of ±21.5m, which may reflect the limited data quality of IGDR without retracking correction of the return-pulse waveform. Drawing orthogonals to the contours, ice drainage basins are determined and they are slightly different from the previous ones defined by the over-snow traverse surveys.
机译:利用SEASAT雷达测高仪的临时地球物理数据记录(IGDR),编制了以30°E和80°E以及纬度72°S为边界的南极冰盖的构造图。该地区沿63条亚卫星地面轨迹,每秒钟采样(相隔6.62公里)总共获得7480个足迹数据。该区域被划分为边长分别为纬度0.1°和经度0.4°的矩形,并且通过SEASAT测高数据得出的海平面上的平均海拔高度用于计算机辅助轮廓。由于冰盖上147个交叉点的高度误差的标准偏差为±6.7m,并且来自坡面效应和其他来源的高度误差为20m,因此对于海拔高于500m的内陆地区,应选择100m的轮廓间隔水平。所获得的配置类似于Scott Polar Research Institute(1983)发布的地图。来自三角测量,卫星多普勒定位和先前发布的地形图的总共157个地面测量数据用于估计获得的配置图的总体准确性。地面勘测高度平均比SEASAT得出的高度低2.2m,标准偏差为±21.5m,这可能反映了IGDR有限的数据质量,而无需对回波波形进行重新跟踪校正。绘制与轮廓线正交的线,确定了排水盆地,它们与过雪遍历调查所定义的先前盆地略有不同。

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