Weigelt Matthias, Jäggi Adrian, Meyer Ulrich, Arnold Daniel, Mayer-Gürr Torsten, Öhlinger Felix, Sośnica Krzysztof, Ebadi Sahar, Schön Steffen, Steffen Holger
Institute for Satellite Geodesy and Inertial Sensing, German Aerospace Center (DLR), Callinstraße 30b, 30167 Hanover, Germany.
Institut für Erdmessung, Leibniz University of Hannover, Schneiderberg 50, 30167 Hanover, Germany.
J Geod. 2024;98(9):84. doi: 10.1007/s00190-024-01888-5. Epub 2024 Sep 13.
The satellite missions GRACE and GRACE Follow-On have undoubtedly been the most important sources to observe mass transport on global scales. Within the Combination Service for Time-Variable Gravity Fields (COST-G), gravity field solutions from various processing centers are being combined to improve the signal-to-noise ratio and further increase the spatial resolution. The time series of monthly gravity field solutions suffer from a data gap of about one year between the two missions GRACE and GRACE Follow-On among several smaller data gaps. We present an intermediate technique bridging the gap between the two missions allowing (1) for a continued and uninterrupted time series of mass observations and (2) to compare, cross-validate and link the two time series. We focus on the combination of high-low satellite-to-satellite tracking (HL-SST) of low-Earth orbiting satellites by GPS in combination with satellite laser ranging (SLR), where SLR contributes to the very low degrees and HL-SST is able to provide the higher spatial resolution at an lower overall precision compared to GRACE-like solutions. We present a complete series covering the period from 2003 to 2022 filling the gaps of GRACE and between the missions. The achieved spatial resolution is approximately 700 km at a monthly temporal resolutions throughout the time period of interest. For the purpose of demonstrating possible applications, we estimate the low degree glacial isostatic adjustment signal in Fennoscandia and North America. In both cases, the location, the signal strength and extend of the signal coincide well with GRACE/GRACE-FO solutions achieving 99.5% and 86.5% correlation, respectively.
GRACE和GRACE后续卫星任务无疑是全球尺度质量传输观测的最重要来源。在时变重力场组合服务(COST-G)中,来自各个处理中心的重力场解正在进行组合,以提高信噪比并进一步提高空间分辨率。月度重力场解的时间序列在GRACE和GRACE后续任务之间存在约一年的数据空白,此外还有几个较小的数据空白。我们提出了一种中间技术,弥合了这两个任务之间的差距,从而(1)实现质量观测的连续不间断时间序列,以及(2)对两个时间序列进行比较、交叉验证和关联。我们专注于通过GPS对低地球轨道卫星进行高低卫星间跟踪(HL-SST)与卫星激光测距(SLR)的组合,其中SLR有助于获取极低阶次信息,而HL-SST能够以低于类似GRACE解的总体精度提供更高的空间分辨率。我们给出了一个完整的序列,涵盖2003年至2022年,填补了GRACE任务期间以及两个任务之间的空白。在整个感兴趣的时间段内,实现的空间分辨率在月度时间分辨率下约为700公里。为了展示可能的应用,我们估计了芬诺斯堪的亚和北美的低阶冰川均衡调整信号。在这两种情况下,信号的位置、强度和范围与GRACE/GRACE-FO解非常吻合,相关性分别达到99.5%和86.5%。