在现代卫星重力任务范围内总储水量大尺度变异性的研究

Jan Mikocki, Artur Lenczuk, J. Bogusz
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摘要

地球重力场变化分析是物理大地测量学的重要任务之一。因此,了解重力场的选择特征是确定地球形状过程的基本要素,有助于找到地球系统质量再分布的信息。自2002年以来,重力恢复与气候实验(GRACE)卫星重力任务及其后续GRACE- fo (GRACE followon)任务成功观测了重力场的变化。本文介绍了GRACE/GRACE- fo观测结果,其中包括mascons的信息,它们由三个处理中心提供:(1)空间研究中心(CSR);(2)喷气推进实验室(JPL;(3)戈达德航天飞行中心(GSFC;美国马里兰州)。在接下来的研究中,我们使用GSFC提供的数据,以全球总储水量(TWS)的分布形式表示,TWS以等效水高(EWH)表示。在我们的研究中,我们专注于识别TWS有显著变化的区域。我们分析了TWS的季节性短期变化,即年振荡幅度(陆地水圈中最明显的振荡)和长期变化,即趋势(气候研究的一个关键参数),使用最小二乘法确定。因此,我们选取了15个具有TWS极端变化特征的区域,即11个区域为年幅值,4个区域为趋势参数。我们在赤道地区(主要是亚马逊河、尼日尔河、恒河、雅鲁藏布江流域地区)和被巨大冰块覆盖的地区(阿拉斯加、格陵兰岛)获得了大于140分钟的季节变化。在南极洲西部、巴塔哥尼亚或里海周围,观测到的储水量变化率最大,为±70。研究结果还强调了人类对大陆水团(如墨西哥、印度河和恒河流域)的重大影响。关键词:GRACE; TWS;陆地水文
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The study of large-scale variability in total water storage within the context of modern satellite gravity missions
The analysis of Earth’s gravity field changes is the one of essential task of physical geodesy. So the knowledge about selected characteristics of gravity field is the basic element of the Earth shape determining process and help to find information about mass redistribution in the Earth system. Since 2002, the gravity field changes have been successfully observed by the Gravity Recovery and Climate Experiment (GRACE) satellite gravity mission and its continued GRACE-FO (GRACE Follow-On) mission. The results obtained from GRACE/GRACE-FO observations are presented, among other, in form of mascons and they are provid-ed by three processing centers: (1) Center for Space Research (CSR; Austin, United States), (2) Jet Propulsion Laboratory (JPL; Pasadena, United States), and (3) Goddard Space Flight Center (GSFC; Maryland, United States). In the following study, we used data provided by GSFC in form of the global distribution of Total Water Storage (TWS), which are expressed in terms of Equivalent Water Height (EWH). In our study, we focused on identifying areas with significant changes in TWS. We analysed TWS fluctuations in seasonal short-term changes, i.e., amplitude of annual oscillation (the most pronounced oscillation in the land hydro-sphere) and longterm changes, i.e., trend (a key parameter for climate studies) determined using the Least Squares Method. As a result, we selected 15 areas characterised by extreme TWS changes, i.e., 11 areas for annual amplitude and 4 areas for trend parameter. We obtained seasonal changes greater than 140 mm in areas within the equator (mainly Amazon, Niger, Ganges, Brahmaputra river basin regions) and areas covered by huge ice masses (Alaska, Greenland). The greatest rate of change in water storage at ±70 is observed around West Antarctica, Patagonia or the Caspian Sea. The results also emphasize the significant human impact in continental water masses (e.g. Mexico, Indus and Ganges river basins). Keywords: GRACE, TWS, land hydrology, gravity missions
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