与GRACE卫星重力任务比较的全球水文模型预测的陆地储水量的多年和年代际变化评估

IF 5.7 1区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY
Julia Pfeffer, Anny Cazenave, Alejandro Blazquez, Bertrand Decharme, Simon Munier, Anne Barnoud
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引用次数: 1

摘要

摘要GRACE(重力恢复和气候实验)卫星重力任务使我们能够对地球系统内的物质运输进行全球监测,从而使我们对气候变化中的全球水循环的理解取得前所未有的进展。本研究的重点是基于GRACE解决方案和两个全球水文模型的集合,对陆地储水量相对于时间平均值的变化进行量化。GRACE卫星重力数据在多年和年代际时间尺度上检测到陆地储水量的显著变化,这些变化虽然与降水一致,但通常被全球水文模型低估。在南美洲(亚马逊河流域、弗朗西斯科河流域和帕拉那河流域)和热带非洲(刚果河流域、赞比西河流域和奥卡万戈河流域)观察到最大的差异(等效水高超过20厘米)。在世界范围内观察到较小但显著的差异(几厘米)。虽然这种差异的起源尚不清楚,但部分原因可能与气候有关,至少部分原因是水文模型的预测不准确。由于不准确的气象强迫(如降水)、未解决的地下水过程、人为影响、不断变化的植被覆盖和有限的校准/验证数据集,全球水文模型确实可能忽略陆地水循环的多年至年代际变化。在本研究中,GRACE卫星测量和水文模型预测之间的显著差异已被确定、量化和表征。必须努力更好地了解多年和年代际时间尺度方法之间的差距,这对利用全球水文模型预测气候变化条件下水资源演变提出了挑战。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Assessment of pluri-annual and decadal changes in terrestrial water storage predicted by global hydrological models in comparison with the GRACE satellite gravity mission
Abstract. The GRACE (Gravity Recovery And Climate Experiment) satellite gravity mission enables global monitoring of the mass transport within the Earth's system, leading to unprecedented advances in our understanding of the global water cycle in a changing climate. This study focuses on the quantification of changes in terrestrial water storage with respect to the temporal average based on an ensemble of GRACE solutions and two global hydrological models. Significant changes in terrestrial water storage are detected at pluri-annual and decadal timescales in GRACE satellite gravity data that are generally underestimated by global hydrological models though consistent with precipitation. The largest differences (more than 20 cm in equivalent water height) are observed in South America (Amazon, São Francisco and Paraná River basins) and tropical Africa (Congo, Zambezi and Okavango River basins). Smaller but significant (a few centimetres) differences are observed worldwide. While the origin of such differences is unknown, part of it is likely to be climate-related and at least partially due to inaccurate predictions of hydrological models. Pluri-annual to decadal changes in the terrestrial water cycle may indeed be overlooked in global hydrological models due to inaccurate meteorological forcing (e.g. precipitation), unresolved groundwater processes, anthropogenic influences, changing vegetation cover and limited calibration/validation datasets. Significant differences between GRACE satellite measurements and hydrological model predictions have been identified, quantified and characterised in the present study. Efforts must be made to better understand the gap between methods at both pluri-annual and decadal timescales, which challenges the use of global hydrological models for the prediction of the evolution of water resources in changing climate conditions.
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来源期刊
Hydrology and Earth System Sciences
Hydrology and Earth System Sciences 地学-地球科学综合
CiteScore
10.10
自引率
7.90%
发文量
273
审稿时长
15 months
期刊介绍: Hydrology and Earth System Sciences (HESS) is a not-for-profit international two-stage open-access journal for the publication of original research in hydrology. HESS encourages and supports fundamental and applied research that advances the understanding of hydrological systems, their role in providing water for ecosystems and society, and the role of the water cycle in the functioning of the Earth system. A multi-disciplinary approach is encouraged that broadens the hydrological perspective and the advancement of hydrological science through integration with other cognate sciences and cross-fertilization across disciplinary boundaries.
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