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Modeling large-scale human alteration of land surface hydrology and climate

机译:模拟人类大规模地表水文学和气候变化

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Abstract Rapidly expanding human activities have profoundly affected various biophysical and biogeochemical processes of the Earth system over a broad range of scales, and freshwater systems are now amongst the most extensively altered ecosystems. In this study, we examine the human-induced changes in land surface water and energy balances and the associated climate impacts using a coupled hydrological–climate model framework which also simulates the impacts of human activities on the water cycle. We present three sets of analyses using the results from two model versions—one with and the other without considering human activities; both versions are run in offline and coupled mode resulting in a series of four experiments in total. First, we examine climate and human-induced changes in regional water balance focusing on the widely debated issue of the desiccation of the Aral Sea in central Asia. Then, we discuss the changes in surface temperature as a result of changes in land surface energy balance due to irrigation over global and regional scales. Finally, we examine the global and regional climate impacts of increased atmospheric water vapor content due to irrigation. Results indicate that the direct anthropogenic alteration of river flow in the Aral Sea basin resulted in the loss of?~510?km_(3) of water during the latter half of the twentieth century which explains about half of the total loss of water from the sea. Results of irrigation-induced changes in surface energy balance suggest a significant surface cooling of up to 3.3?K over 1° grids in highly irrigated areas but a negligible change in land surface temperature when averaged over sufficiently large global regions. Results from the coupled model indicate a substantial change in 2?m air temperature and outgoing longwave radiation due to irrigation, highlighting the non-local (regional and global) implications of irrigation. These results provide important insights on the direct human alteration of land surface water and energy balances, highlighting the need to incorporate human activities such as irrigation into the framework of global climate models and Earth system models for better prediction of future changes under increasing human influence and continuing global climate change.
机译:摘要人类活动的迅速扩展已在广泛的范围内深刻影响着地球系统的各种生物物理和生物地球化学过程,而淡水系统现已成为变化最为广泛的生态系统之一。在这项研究中,我们使用耦合的水文-气候模型框架研究了人为引起的地表水和能量平衡的变化以及相关的气候影响,该框架还模拟了人类活动对水循环的影响。我们使用两个模型版本的结果提供了三组分析-一组带有模型,另一组没有考虑人类活动。这两个版本均以脱机和耦合模式运行,总共进行了四个实验。首先,我们研究气候和人为因素引起的区域水平衡的变化,重点是中亚咸海干燥问题。然后,我们讨论了由于全球和区域尺度上的灌溉而导致的地表能量平衡变化导致地表温度的变化。最后,我们研究了由于灌溉而增加的大气水蒸气含量对全球和区域气候的影响。结果表明,在咸海流域,人为直接改变的河流流量导致在20世纪后半叶损失了约510 kmkm(3)的水,这解释了大约50%的总水损失。海。灌溉引起的表面能平衡变化的结果表明,在高度灌溉的区域中,超过1°网格的地表温度最高可降低3.3?K,但在足够大的全球区域平均时,地表温度的变化可忽略不计。耦合模型的结果表明,由于灌溉,气温升高了2?m,长波辐射发生了实质性变化,突显了灌溉对非本地(区域和全球)的影响。这些结果提供了有关人类直接改变土地表层水和能量平衡的重要见解,强调了将诸如灌溉等人类活动纳入全球气候模型和地球系统模型框架的必要性,以便更好地预测在人类影响和日趋增加的情况下的未来变化。持续的全球气候变化。

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