影响尺度的水文预报:德国0.6公里气候弹性水资源管理的综合ParFlow水文模型

IF 2.6 Q2 WATER RESOURCES
Alexandre Belleflamme, K. Goergen, N. Wagner, S. Kollet, S. Bathiany, Juliane El Zohbi, D. Rechid, J. Vanderborght, H. Vereecken
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引用次数: 0

摘要

在过去几年(2018-202022年)影响中欧的反复干旱背景下,基于陆地水循环现状的及时信息和对其演变的预测,对水资源进行气候适应性管理变得越来越重要。为了实现这一点,我们提出了一种新的设置,用于在德国和邻近地区使用高时空分辨率(即0.611公里,每小时时间步长)的综合水文模型ParFlow/CLM模拟陆地水循环。我们表明,这种设置可以作为监测和预测系统的基础,该系统旨在为许多部门的利益相关者,尤其是农业部门的利益攸关者提供诊断和指标,突出地表水状态和通量的不同方面,如地表水储存、渗透水、毛细管上升,或不同(根)深度的植物可用水的部分。利用2011-2020年期间每月基于观测的数据对新的模拟设置进行验证,对于此处分析的陆地水循环的所有主要组成部分,即体积土壤湿度、蒸散、地下水位深度和河流流量,都产生了良好的结果。由于这种设置依赖于标准化的网格定义和最近全球可用的静态场和参数(例如,地形、土壤水力特性、土地覆盖),因此工作流程可以很容易地转移到地球的许多区域,包括测量稀疏的区域,因为ParFlow/CLM不需要校准。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Hydrological forecasting at impact scale: the integrated ParFlow hydrological model at 0.6 km for climate resilient water resource management over Germany
In the context of the repeated droughts that have affected central Europe over the last years (2018–2020, 2022), climate-resilient management of water resources, based on timely information about the current state of the terrestrial water cycle and forecasts of its evolution, has gained an increasing importance. To achieve this, we propose a new setup for simulations of the terrestrial water cycle using the integrated hydrological model ParFlow/CLM at high spatial and temporal resolution (i.e., 0.611 km, hourly time step) over Germany and the neighboring regions. We show that this setup can be used as a basis for a monitoring and forecasting system that aims to provide stakeholders from many sectors, but especially agriculture, with diagnostics and indicators highlighting different aspects of subsurface water states and fluxes, such as subsurface water storage, seepage water, capillary rise, or fraction of plant available water for different (root-)depths. The validation of the new simulation setup with observation-based data monthly over the period 2011–2020 yields good results for all major components of the terrestrial water cycle analyzed here, i.e., volumetric soil moisture, evapotranspiration, water table depth, and river discharge. As this setup relies on a standardized grid definition and recent globally available static fields and parameters (e.g., topography, soil hydraulic properties, land cover), the workflow could easily be transferred to many regions of the Earth, including sparsely gauged regions, since ParFlow/CLM does not require calibration.
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来源期刊
Frontiers in Water
Frontiers in Water WATER RESOURCES-
CiteScore
4.00
自引率
6.90%
发文量
224
审稿时长
13 weeks
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