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New Antarctic Gravity Anomaly Grid for Enhanced Geodetic and Geophysical Studies in Antarctica

机译:新的南极重力异常网格用于增强南极的大地测量和地球物理研究

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摘要

Gravity surveying is challenging in Antarctica because of its hostile environment and inaccessibility. Nevertheless, many ground-based, airborne and shipborne gravity campaigns have been completed by the geophysical and geodetic communities since the 1980s. We present the first modern Antarctic-wide gravity data compilation derived from 13 million data points covering an area of 10 million km2, which corresponds to 73% coverage of the continent. The remove-compute-restore technique was applied for gridding, which facilitated levelling of the different gravity datasets with respect to an Earth Gravity Model derived from satellite data alone. The resulting free-air and Bouguer gravity anomaly grids of 10 km resolution are publicly available. These grids will enable new high-resolution combined Earth Gravity Models to be derived and represent a major step forward towards solving the geodetic polar data gap problem. They provide a new tool to investigate continental-scale lithospheric structure and geological evolution of Antarctica.
机译:由于南极的敌对环境和交通不便,重力测量在南极具有挑战性。然而,自1980年代以来,地球物理和大地测量界已经完成了许多地面,空中和舰载重力运动。我们提出了第一个现代南极范围的重力数据汇编,该数据汇编来自1300万个数据点,覆盖了1000万公里 2 ,相当于该大陆的73%覆盖率。删除-计算-恢复技术被应用于网格化,这有助于相对于仅从卫星数据得出的地球重力模型进行不同重力数据集的水准测量。由此产生的10 km分辨率的自由空气和布格重力异常网格是公开可用的。这些网格将能够推导出新的高分辨率组合地球重力模型,代表着朝着解决大地极地数据间隙问题迈出的重要一步。它们为研究南极大陆规模的岩石圈结构和地质演化提供了新的工具。

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