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Guidelines for cold‐regions groundwater numerical modeling

机译:冷区地下水数值建模指南

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Abstract The impacts of ongoing climate warming on cold‐regions hydrogeology and groundwater resources have created a need to develop groundwater models adapted to these environments. Although permafrost is considered relatively impermeable to groundwater flow, permafrost thaw may result in potential increases in surface water infiltration, groundwater recharge, and hydrogeologic connectivity that can impact northern water resources. To account for these feedbacks, groundwater models that include the dynamic effects of freezing and thawing on ground properties and thermal regimes have been recently developed. However, these models are more complex than traditional hydrogeology numerical models due to the inclusion of nonlinear freeze–thaw processes and complex thermal boundary conditions. As such, their use to date has been limited to a small community of modeling experts. This article aims to provide guidelines and tips on cold‐regions groundwater modeling for those with previous modeling experience. This article is categorized under: Engineering Water > Methods Science of Water > Hydrological Processes
机译:摘要持续的气候变暖对冷区水文地质和地下水资源的影响已经引起了开发适合这些环境的地下水模型的需求。尽管永久冻土被认为是地下水流动相对不渗透的,但永久冻结可能会导致地表水浸润,地下水补给和水理连通性的潜在增加,这可能会影响北方水资源。为了解决这些反馈,最近已经开发了包括冷冻和解冻对地面特性和热度机制的动态影响的地下水模型。但是,由于包括非线性冻结过程和复杂的热边界条件,这些模型比传统水文地质学模型更为复杂。因此,迄今为止,它们的使用仅限于一个小的建模专家社区。本文旨在为具有以前建模经验的人提供有关冷区域地下水建模的指南和技巧。本文分类为:工程水>水科学>水文过程

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