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Confirming regional 1 cm differential geoid accuracy from airborne gravimetry: the Geoid Slope Validation Survey of 2011

机译:通过空中重力法确认区域1 cm大地水准面的精度:2011年大地水准面坡度验证调查

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摘要

A terrestrial survey, called the Geoid Slope Validation Survey of 2011 (GSVS11), encompassing leveling, GPS, astrogeodetic deflections of the vertical (DOV) and surface gravity was performed in the United States. The general purpose of that survey was to evaluate the current accuracy of gravimetric geoid models, and also to determine the impact of introducing new airborne gravity data from the 'Gravity for the Redefinition of the American Vertical Datum' (GRAV-D) project. More specifically, the GSVS11 survey was performed to determine whether or not the GRAV-D airborne gravimetry, flown at 11 km altitude, can reduce differential geoid error to below 1 cm in a low, flat gravimetrically uncomplicated region. GSVS11 comprises a 325 km traverse from Austin to Rockport in Southern Texas, and includes 218 GPS stations (σΔh = 0.4 cm over any distance from 0.4 to 325 km) co-located with first-order spirit leveled orthomet-ric heights (σΔh = 1-3 cm end-to-end), including new surface gravimetry, and 216 astronomically determined vertical deflections (σDOV=0.1"). The terrestrial survey data were compared in various ways to specific geoid models, including analysis of RMS residuals between all pairs of points on the line, direct comparison of DOVs to geoid slopes, and a harmonic analysis of the differences between the terrestrial data and various geoid models. These comparisons of the terrestrial survey data with specific geoid models showed conclusively that, in this type of region (low, flat) the geoid models computed using existing terrestrial gravity, combined with digital elevation models (DEMs) and GRACE and GOCE data, differential geoid accuracy of 1 to 3 cm (1 σ) over distances from 0.4 to 325 km were currently being achieved. However, the addition of a contemporaneous airborne gravity data set, flown at 11 km altitude, brought the estimated differential geoid accuracy down to 1 cm over nearly all distances from 0.4 to 325 km.
机译:在美国进行了一项称为2011年大地水准面验证调查(GSVS11)的地面调查,包括水准仪,GPS,垂直方向(DOV)的天文大地挠度和表面重力。该调查的总体目的是评估重力大地水准面模型的当前准确性,并确定从“重新定义美国垂直基准重力”(GRAV-D)项目引入新的空中重力数据的影响。更具体地说,进行了GSVS11调查,以确定在低而平坦的重量简单区域中,以11 km高空飞行的GRAV-D空中重量分析仪是否可以将大地水准面误差减小到1 cm以下。 GSVS11包括从得克萨斯州南部到奥斯汀到洛克波特的325公里横断面,并包括218个GPS站(在0.4到325公里之间的任何距离上,σΔh= 0.4厘米)与一阶水平水准正高(σΔh= 1 -3 cm端到端),包括新的表面重力法,以及216个天文学确定的垂直偏转(σDOV= 0.1“)。以各种方式将地面调查数据与特定的大地水准面模型进行了比较,包括分析所有两对之间的RMS残差线上的点数,DOV与大地水准面坡度的直接比较,以及对地面数据与各种大地水准面模型之间差异的谐波分析,这些对地面勘测数据与特定大地水准面模型的比较表明,在这种类型的区域中(低,平坦)使用现有地面重力计算的大地水准面模型,结合数字高程模型(DEM)以及GRACE和GOCE数据,在0.4至3的距离上,大地水准面精度为1至3 cm(1σ)目前正在达到25公里。但是,增加了一个同时空载重力数据集,该数据集飞行在11 km的高度上,使得从0.4到325 km的几乎所有距离上估计的大地水准面精度都降低到1 cm。

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