Liu Yongxin, Fok Hok Sum, Tenzer Robert, Chen Qiang, Chen Xiuwan
School of Earth and Space Sciences, Peking University, Beijing 100871, China.
Engineering Research Center of Earth Observation and Navigation (CEON), Ministry of Education of the PRC, No. 5 Yiheyuan Road, Haidian District, Beijing 100871, China.
Entropy (Basel). 2019 Jul 7;21(7):664. doi: 10.3390/e21070664.
Global navigation satellite systems (GNSS) techniques, such as GPS, can be used to accurately record vertical crustal movements induced by seasonal terrestrial water storage (TWS) variations. Conversely, the TWS data could be inverted from GPS-observed vertical displacement based on the well-known elastic loading theory through the Tikhonov regularization (TR) or the Helmert variance component estimation (HVCE). To complement a potential non-uniform spatial distribution of GPS sites and to improve the quality of inversion procedure, herein we proposed in this study a novel approach for the TWS inversion by jointly supplementing GPS vertical crustal displacements with minimum usage of external TWS-derived displacements serving as pseudo GPS sites, such as from satellite gravimetry (e.g., Gravity Recovery and Climate Experiment, GRACE) or from hydrological models (e.g., Global Land Data Assimilation System, GLDAS), to constrain the inversion. In addition, Akaike's Bayesian Information Criterion (ABIC) was employed during the inversion, while comparing with TR and HVCE to demonstrate the feasibility of our approach. Despite the deterioration of the model fitness, our results revealed that the introduction of GRACE or GLDAS data as constraints during the joint inversion effectively reduced the uncertainty and bias by 42% and 41% on average, respectively, with significant improvements in the spatial boundary of our study area. In general, the ABIC with GRACE or GLDAS data constraints displayed an optimal performance in terms of model fitness and inversion performance, compared to those of other GPS-inferred TWS methodologies reported in published studies.
全球导航卫星系统(GNSS)技术,如GPS,可用于精确记录季节性陆地水储量(TWS)变化引起的地壳垂直运动。相反,基于著名的弹性加载理论,可通过蒂霍诺夫正则化(TR)或赫尔默特方差分量估计(HVCE)从GPS观测到的垂直位移中反演TWS数据。为了补充GPS站点潜在的非均匀空间分布并提高反演程序的质量,在本研究中,我们提出了一种新的TWS反演方法,即通过以最少使用外部TWS衍生位移(如来自卫星重力测量(例如重力恢复与气候实验,GRACE)或水文模型(例如全球陆地数据同化系统,GLDAS))作为伪GPS站点来联合补充GPS地壳垂直位移,以约束反演。此外,在反演过程中采用了赤池贝叶斯信息准则(ABIC),同时与TR和HVCE进行比较,以证明我们方法的可行性。尽管模型拟合度有所下降,但我们的结果表明,在联合反演过程中引入GRACE或GLDAS数据作为约束,平均有效降低了不确定性和偏差,分别降低了42%和41%,并且在我们研究区域的空间边界方面有显著改善。总体而言,与已发表研究中报道的其他GPS推断TWS方法相比,带有GRACE或GLDAS数据约束的ABIC在模型拟合度和反演性能方面表现出最佳性能。