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Impacts of future land cover and climate changes on runoff in the mostly afforested river basin in North China

机译:未来陆地覆盖与气候变化对华北大多数富裕河流河流域径流影响的影响

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The Luanhe River basin, the mostly afforested river basin in North China, has exhibited significant land use/land cover change (LUCC) under climate change that could jointly affect water availability of the basin in the future. This study examines both impacts of LUCC and climate change on runoff over the upper reaches of the Luanhe River basin. First, the land use in 2020 is predicted based on the Cellular Automata-Markov (CA-Markov). Second, a hydrological model (Soil Water Assessment Tools, SWAT) is set up for the baseline period 1961-1979 and driven primarily by outputs from five general circulation models (GCMs) under four representative concentration pathways (RCPs) (i.e., RCP2.6, RCP4.5, RCP6.0 and RCP8.5) for the period 2020-2030. Results show that the ensemble mean annual precipitation may increase under four RCPs for the period 2020-2030, with the maximum (470 mm/yr) and minimum (444 mm/yr) for RCP8.5 and RCP6.0, respectively, 1-7% higher than the observed mean annual precipitation (441 mm/yr) during 1961-1979. The relationship between the runoff simulations and the RCPs under the 2020 land use scenario is nonlinear, with the maximum (57 mm/yr) and minimum (50 mm/yr) mean annual runoff depths under the RCP4.5 and RCP6.0 scenarios, respectively, similar to 58% and similar to 39% higher than the mean annual observed runoff depth (36 mm/yr) for the baseline period. The increase in forestland (similar to 56%) and decrease in agriculture land (similar to -30%) are remarkable for the period 1970-2020, driven primarily by afforestation implemented in the Luanhe River basin. LUCC would lead to a slight decrease in mean annual runoff, and the runoff only increases in summer but decreases in other three seasons. The decrease in surface runoff and groundwater discharge jointly results in the overall decrease in runoff due to LUCC. In general, the climate change impact will dominate runoff change for the study basin, though marked afforestation has taken place and is
机译:滦河流域,北华北大多数富裕的河流盆地,在气候变化下表现出大量的土地使用/土地覆盖变化(LUCC),可共同影响未来盆地的水资源可用性。本研究审查了Lucc和气候变化对滦河流域上游径流的影响。首先,基于蜂窝自动机 - 马尔可夫(CA-Markov)预测2020年的土地使用。其次,水文模型(土壤水评估工具,SWAT)设置为基线1961-1979,并主要由四个代表性浓度途径(RCP)(即RCP2.6)的五种通用循环模型(GCMS)的产出驱动,rcp4.5,rcp6.0和rcp8.5)在2020-2030期间。结果表明,集成的平均年降水量在2020 - 2030年期间的四个RCP下可能会增加,最大(470mm / Yr)和最小(474 mm / Yr),分别为RCP8.5,1-比观察到的平均年降水量高7%(441 mm / YR)。径流模拟与2020土地使用场景下的RCP之间的关系是非线性的,最大(57 mm / yr)和最小(50 mm / yr)均值在RCP4.5和RCP6.0场景下的年径流深度,分别与58%相似,与基线期间的平均年度观察到的径流深度(36 mm / YR)高出39%。 1970 - 2010年期间,林地的增加(类似于56%)和农业土地减少(类似于-30%),主要是在滦河流域实施的造林中推动。 Lucc将导致平均年径流略微下降,径流仅在夏季增加,但其他三季差价。表面径流和地下水排放的降低连续导致由于LUCC引起的径流的总体下降。一般而言,气候变化影响将对研究盆地的径流变化占主导地位,虽然已经进行了标记的造林并是

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