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首页> 外文期刊>Hydrology and Earth System Sciences >Evapotranspiration in the Amazon: spatial patterns, seasonality, and recent trends in observations, reanalysis, and climate models
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Evapotranspiration in the Amazon: spatial patterns, seasonality, and recent trends in observations, reanalysis, and climate models

机译:亚马逊的蒸散:空间模式,季节性,观察,重新分析和气候模型的近期趋势

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Water recycled through transpiring forests influences the spatial distribution of precipitation in the Amazon and has been shown to play a role in the initiation of the wet season. However, due to the challenges and costs associated with measuring evapotranspiration (ET) directly and high uncertainty in remote-sensing ET retrievals, the spatial and temporal patterns in Amazon ET remain poorly understood. In this study, we estimated ET over the Amazon and 10 sub-basins using a catchment-balance approach, whereby ET is calculated directly as the balance between precipitation, runoff, and change in groundwater storage. We compared our results with ET from remote-sensing datasets, reanalysis, models from Phase?5 and Phase?6 of the Coupled Model Intercomparison Projects (CMIP5 and CMIP6 respectively), and in?situ flux tower measurements to provide a comprehensive overview of current understanding. Catchment-balance analysis revealed a gradient in ET from east to west/southwest across the Amazon Basin, a strong seasonal cycle in basin-mean ET primarily controlled by net incoming radiation, and no trend in ET over the past 2?decades. This approach has a degree of uncertainty, due to errors in each of the terms of the water budget; therefore, we conducted an error analysis to identify the range of likely values. Satellite datasets, reanalysis, and climate models all tended to overestimate the magnitude of ET relative to catchment-balance estimates, underestimate seasonal and interannual variability, and show conflicting positive and negative trends. Only two out of six satellite and model datasets analysed reproduced spatial and seasonal variation in Amazon ET, and captured the same controls on ET as indicated by catchment-balance analysis. CMIP5 and CMIP6 ET was inconsistent with catchment-balance estimates over all scales analysed. Overall, the discrepancies between data products and models revealed by our analysis demonstrate a need for more ground-based ET measurements in the Amazon as well as a need to substantially improve model representation of this fundamental component of the Amazon hydrological cycle.
机译:通过传递森林再循环的水影响了亚马逊降水的空间分布,并且已被证明在潮湿季节的启动中发挥作用。然而,由于与蒸散蒸散(ET)直接相关的挑战和成本,遥感ET检索中的高不确定性,亚马逊ET中的空间和时间图案仍然明白。在这项研究中,我们估计了使用集水平衡方法的亚马逊和10个子盆地,从而直接计算降水,径流和地下水存储中的变化之间的平衡。我们将结果与ET从遥感数据集,再分析,来自耦合型号的阶段互相竞争项目(CMIP5和CMIP6的相位的型号(CMIP5和CMIP6)进行了比较了。理解。集水区分平衡分析显示了亚马逊盆地的Ett到西/西南西南的梯度,这是一个强大的季节性循环,主要由净传入辐射控制,而不是在过去的2年内et et ord et趋势。由于水预算的每个条款中,这种方法具有一定程度的不确定性;因此,我们进行了错误分析,以确定可能的值的范围。卫星数据集,再分析和气候模型均倾向于高估ET的幅度相对于集水区余额,低估季节性和际变异性,并表现出相互矛盾的正负趋势。只有六种卫星和模型数据集中只有两个分析了亚马逊ET的再现空间和季节变化,并捕获了相同的对等控制,如集水平衡分析所示。 CMIP5和CMIP6等与分析的所有尺度的集水平衡估计不一致。总体而言,我们的分析所揭示的数据产品和模型之间的差异表明,在亚马逊中需要更多地基于基于的ET测量,并且需要大大提高亚马逊水文循环的这一基本组件的模型表示。

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