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Hydrological impacts of global land cover change and human water use

机译:全球土地覆盖变化和人类用水的水文影响

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Human impacts on global terrestrial hydrology have been accelerating during the 20th century. These human impacts include the effects of reservoir building and human water use, as well as land cover change. To date, many global studies have focussed on human water use, but only a few focus on or include the impact of land cover change. Here we use PCR-GLOBWB, a combined global hydrological and water resources model, to assess the impacts of land cover change as well as human water use globally in different climatic zones. Our results show that land cover change has a strong effect on the global hydrological cycle, on the same order of magnitude as the effect of human water use (applying irrigation, abstracting water, for industrial use for example, including reservoirs, etc.). When globally averaged, changing the land cover from that of 1850 to that of 2000 increases discharge through reduced evapotranspiration. The effect of land cover change shows large spatial variability in magnitude and sign of change depending on, for example, the specific land cover change and climate zone. Overall, land cover effects on evapotranspiration are largest for the transition of tall natural vegetation to crops in energy-limited equatorial and warm temperate regions. In contrast, the inclusion of irrigation, water abstraction and reservoirs reduces global discharge through enhanced evaporation over irrigated areas and reservoirs as well as through water consumption. Hence, in some areas land cover change and water distribution both reduce discharge, while in other areas the effects may partly cancel out. The relative importance of both types of impacts varies spatially across climatic zones. From this study we conclude that land cover change needs to be considered when studying anthropogenic impacts on water resources.
机译:在20世纪,人类对全球陆地水文学的影响一直在加速。这些对人类的影响包括水库建设和人类用水以及土地覆盖变化的影响。迄今为止,许多全球研究都集中在人类用水上,但只有少数研究集中在或包括了土地覆被变化的影响。在这里,我们使用PCR-GLOBWB(一种综合的全球水文和水资源模型)来评估全球不同气候区域的土地覆盖变化以及人类用水的影响。我们的结果表明,土地覆被变化对全球水文循环有很强的影响,其幅度与人类用水的影响相同(应用灌溉,取水,例如用于工业用途,包括水库等)。如果将全球平均水平从1850年的土地覆盖率更改为2000年的土地覆盖率,可以通过减少蒸散量来增加排放量。土地覆盖变化的影响显示出很大的空间变异性,并且变化的迹象取决于例如特定的土地覆盖变化和气候带。总体而言,土地覆盖对蒸散量的影响最大,是在能量有限的赤道和温带地区向高大的自然植被过渡到农作物。相比之下,灌溉,取水和水库的纳入通过增加灌溉区和水库的蒸发量以及水的消耗减少了全球排放量。因此,在某些地区,土地覆盖的变化和水的分布都减少了排放,而在其他地区,这种影响可能会部分抵消。两种类型的影响的相对重要性在不同的气候区域在空间上有所不同。根据这项研究,我们得出结论,在研究人为因素对水资源的影响时,需要考虑土地覆被变化。

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