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USING A MOBILE RADIO ECHO SOUNDER TO MEASURE BEDROCK TOPOGRAPHY IN EAST QUEEN MAUD LAND, ANTARCTICA

机译:使用移动无线电回声测深仪测量南极洲东部女王地区的地形测量

摘要

As part of the Dome-Fuji Project, the topography of the bedrock over a wide area around Dome-F and along routes from Dome-F to S16 (about 1000 km distance) was surveyed by radio echo sounder with a continuous recording system. The bedrock topography was successfully measured under ice sheets thicker than 3500m, and the performance of the radio echo sounder was confirmed. The highest point of Dome-F was located in the basin like topography of the bedrock, surrounded by more elevated areas. The strength of the bedrock echo were found to differ substantially between inside and outside of the Dome-F area. This difference is probably due to the difference of ice sheet temperatures between these areas, because the attenuation coefficients depend on the ice temperature. The stronger echo at high altitude will enable us to measure ice thickness more than 3500 m.
机译:作为Dome-Fuji项目的一部分,通过带有连续记录系统的无线电回波测深仪对Dome-F周围宽阔区域以及从Dome-F到S16的路线(约1000公里距离)的基岩地形进行了测量。在厚度大于3500m的冰盖下成功地测量了基岩地形,并证实了无线电回波测深仪的性能。 Dome-F的最高点位于盆地中,就像基岩的地形一样,被更高的区域所包围。发现在Dome-F区域的内部和外部之间,基岩回波的强度存在很大差异。这种差异可能是由于这些区域之间冰盖温度的差异所致,因为衰减系数取决于冰温。高空回波更强将使我们能够测量超过3500 m的冰厚。

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