A conceptual approach for assessing the impact of climate change on groundwater and related surface waters in cold regions (Finland)Une approche conceptuelle pour évaluer les impacts du changement climatique sur les eaux souterraines et sur les eaux de surface dont elles dependent dans des régions froides (Finlande)Un enfoque conceptual para la evaluación de los impactos de cambios climáticos en las aguas subterráneas y aguas superficiales relacionadas en regiones frías (Finlandia)评价气候变化对寒冷地区 (芬兰) 地下水和相关地表水影响的概念性方法Uma abordagem conceptual para a avaliação do impacte das alterações climáticas nas águas subterrâneas e águas superficiais inter-relacionadas em regiões frias (Finlândia)

被引:0
|
作者
Jarkko Okkonen
Mikko Jyrkama
Bjørn Kløve
机构
[1] University of Oulu,Water Resources and Environmental Engineering Laboratory, Department of Process and Environmental Engineering
[2] University of Waterloo,Department of Civil and Environmental Engineering
关键词
Climate change; Esker; Groundwater/surface-water relations; Boreal environment; Finland;
D O I
10.1007/s10040-009-0529-9
中图分类号
学科分类号
摘要
A literature review of the impacts of anticipated climate change on unconfined aquifers is presented, along with a conceptual framework for evaluating the complex responses of surface and subsurface hydrology to climate variables in cold regions. The framework offers a way to conceptualize how changes in one component of the system may impact another by delineating the relationships among climate drivers, hydrological responses, and groundwater responses in a straight-forward manner. The model is elaborated in the context of shallow unconfined aquifers in the boreal environment of Finland. In cold conditions, climate change is expected to reduce snow cover and soil frost and increase winter floods. The annual surface water level maximum will occur earlier in spring, and water levels will decrease in summer due to higher evapotranspiration rates. The maximum recharge and groundwater level are expected to occur earlier in the year. Lower groundwater levels are expected in summer due to higher evapotranspiration rates. The flow regimes between shallow unconfined aquifers and surface water may change, affecting water quantity and quality in the surface and groundwater systems.
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页码:429 / 439
页数:10
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