How realistic are multi-decadal reconstructions of GRACE-like total water storage anomalies?

IF 5.9 1区 地球科学 Q1 ENGINEERING, CIVIL Journal of Hydrology Pub Date : 2024-10-24 DOI:10.1016/j.jhydrol.2024.132180
Charlotte Hacker, Jürgen Kusche
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Abstract

Reconstructions allow us to extend the Gravity Recovery And Climate Experiment (GRACE) data record into the past and bridge the one-year gap between GRACE and its successor, GRACE-FO (Follow on). Reconstructed total water storage anomalies (TWSA) are obtained by identifying relations between GRACE-derived TWSA and climate variables via statistical and machine learning techniques. However, a comparative analysis of the characteristics and realism of reconstructions is missing.
In this contribution, we close this gap by comparing three global reconstructions by Humphrey and Gudmundsson (2019), Li et al. (2021) and Chandanpurkar et al. (2022) mutually and against output from the Water Global Analysis and Prognosis (WaterGAP) hydrological model from 1979 onwards, against large-scale mass-change derived from geodetic satellite laser ranging (SLR) from 1992 onwards, and finally against differing GRACE and GRACE-FO solutions from 2002 onwards. The reconstructions vary regarding design and trained GRACE solution.
Reconstructions recover the TWSA signal for humid climate regions but disagree for arid climate regions, which is evident on the inter-annual timescales. At seasonal and sub-seasonal timescales, the reconstructions agree surprisingly well in many regions. Our comparison against independent SLR data reveals that reconstructions (only) partially succeed in representing anomalous TWSA for areas that are influenced by significant climate modes such as El Niño-Southern Oscillation (ENSO).
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类似于 GRACE 的总蓄水异常的十年期重建的现实性如何?
重构使我们能够将重力恢复与气候实验(GRACE)的数据记录延伸到过去,并弥补 GRACE 与其后继者 GRACE-FO(后续)之间的一年差距。通过统计和机器学习技术确定 GRACE 得出的总蓄水量异常与气候变量之间的关系,就可以得到重建的总蓄水量异常(TWSA)。在这篇论文中,我们通过比较 Humphrey 和 Gudmundsson(2019 年)、Li 等人(2021 年)以及 Chandanpurkar 等人(2022 年)的三个全球重建结果,并将其与 GRACE 的输出结果进行对比,弥补了这一空白。(2022 年)的三个全球重建结果相互比较,并与 1979 年以来全球水分析和预测(WaterGAP)水文模型的输出结果、1992 年以来大地测量卫星激光测距(SLR)得出的大尺度质量变化结果以及 2002 年以来不同的 GRACE 和 GRACE-FO 解决方案进行比较。重建结果在湿润气候地区恢复了 TWSA 信号,但在干旱气候地区则不尽相同,这在年际时间尺度上非常明显。在季节和亚季节时间尺度上,许多地区的重建结果惊人地一致。我们与独立的 SLR 数据进行比较后发现,对于受厄尔尼诺-南方涛动(ENSO)等重要气候模式影响的地区,重建(仅)部分成功地代表了异常 TWSA。
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来源期刊
Journal of Hydrology
Journal of Hydrology 地学-地球科学综合
CiteScore
11.00
自引率
12.50%
发文量
1309
审稿时长
7.5 months
期刊介绍: The Journal of Hydrology publishes original research papers and comprehensive reviews in all the subfields of the hydrological sciences including water based management and policy issues that impact on economics and society. These comprise, but are not limited to the physical, chemical, biogeochemical, stochastic and systems aspects of surface and groundwater hydrology, hydrometeorology and hydrogeology. Relevant topics incorporating the insights and methodologies of disciplines such as climatology, water resource systems, hydraulics, agrohydrology, geomorphology, soil science, instrumentation and remote sensing, civil and environmental engineering are included. Social science perspectives on hydrological problems such as resource and ecological economics, environmental sociology, psychology and behavioural science, management and policy analysis are also invited. Multi-and interdisciplinary analyses of hydrological problems are within scope. The science published in the Journal of Hydrology is relevant to catchment scales rather than exclusively to a local scale or site.
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