智利半干旱安第斯山脉水源系统的概念水文模型

IF 3 3区 地球科学 Q2 GEOGRAPHY, PHYSICAL
Gonzalo Navarro, S. MacDonell, Rémi Valois
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引用次数: 4

摘要

半干旱的安第斯山脉源头是智利中北部水文系统的关键组成部分,因为这是支持下游生态系统和人口的径流的主要来源。本研究基于对该地区已发表研究现状的综合批判性分析,开发了智利半干旱安第斯山脉源头的概念性水文模型。我们将大量的文献集中在孤立的水文单元上,包括关于冰川和积雪水文过程的大量文献,以及关于永久冻土地貌、地下水动力学和其他水文特征的较少的文献。除此之外,我们还发现了与多年冻土区的水文地貌及其与地下水的相互作用以及深层含水层补给和循环有关的重要知识空白。为了更好地约束集水区对与冰川和降水减少有关的未来气候情景的响应的模型预测,这两个研究课题是必要的下一步。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
A conceptual hydrological model of semiarid Andean headwater systems in Chile
Semiarid Andean headwaters are key components of the hydrological system of north-central Chile as this is the main source of runoff which supports ecosystems and population located downstream. This study develops a conceptual hydrological model of the Chilean semiarid Andes headwaters, based on an integrative critical analysis of the current state of published research in the region. We combine a plethora of literature focused on isolated hydrological units including extensive literature on glacier and snowpack hydrological processes and less abundant literature on permafrost landforms, groundwater dynamics and other hydrological features. Among others, we identify important knowledge gaps related to the hydrogeomorphological understanding of permafrost area and its interaction with groundwater, as well as deep aquifer recharge and circulation. These two research topics are necessary next steps to better constrain model predictions of catchment response to future climatic scenarios associated with decreasing water contribution from glaciers and precipitation.
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来源期刊
CiteScore
7.20
自引率
5.10%
发文量
53
审稿时长
>12 weeks
期刊介绍: Progress in Physical Geography is a peer-reviewed, international journal, encompassing an interdisciplinary approach incorporating the latest developments and debates within Physical Geography and interrelated fields across the Earth, Biological and Ecological System Sciences.
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