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Evaluation of root water uptake in the ISBA-A-gs land surface model using agricultural yield statistics over France

机译:法国农业收益统计学伊尔巴-A-GS陆地表面模型对根水吸收的评价

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The simulation of root water uptake in land surface models is affected by large uncertainties. Thedifficulty in mapping soil depth and in describing the capacity of plants todevelop a rooting system is a major obstacle to the simulation of theterrestrial water cycle and to the representation of the impacts of drought.In this study, long time series of agricultural statistics are used toevaluate and constrain root water uptake models. The inter-annual variabilityof cereal grain yield and permanent grassland dry matter yield is simulatedover France by the Interactions between Soil, Biosphere and Atmosphere,CO2-reactive (ISBA-A-gs) generic land surface model (LSM). The two soilprofile schemes available in the model are used to simulate the above-groundbiomass (Bag) of cereals and grasslands: a two-layerforce–restore (FR-2L) bulk reservoir model and a multi-layer diffusion (DIF)model. The DIF model is implemented with or without deep soil layers belowthe root zone. The evaluation of the various root water uptake models isachieved by using the French agricultural statistics of Agreste over the1994–2010 period at 45 cropland and 48 grassland départements, for arange of rooting depths. The number of départements where the simulatedannual maximum Bag presents a significant correlation with theyield observations is used as a metric to benchmark the root water uptakemodels. Significant correlations (p value < 0.01) are found for up to29 and 77% of the départements for cereals and grasslands,respectively. A rather neutral impact of the most refined versions of themodel is found with respect to the simplified soil hydrology scheme. Thisshows that efforts should be made in future studies to reduce other sourcesof uncertainty, e.g. by using a more detailed soil and root density profiledescription together with satellite vegetation products. It is found thatmodelling additional subroot-zone base flow soil layers does not improve (andmay even degrade) the representation of the inter-annual variability of thevegetation above-ground biomass. These results are particularly robust forgrasslands, as calibrated simulations are able to represent the extreme 2003and 2007 years corresponding to unfavourable and favourable fodderproduction, respectively.
机译:陆地表面模型的根水摄取的模拟受到大不确定性的影响。在映射土壤深度和描述植物待办事件的能力生根系统中的临床是对题的水循环模拟的主要障碍,以及干旱的影响。在这项研究中,长时间的农业统计数据用于转义为向量并限制根水摄取模型。谷物产量和永久草地干物质收益率的年间变化性是通过土壤,生物圈和大气之间的相互作用,CO 2 - 反应(ISBA-A-GS)通用陆地模型( LSM)。该模型中可用的两种可用的土壤预制方案用于模拟谷物和草原的上述基因( B Ag ):双层恢复(FR-2L)散装储层模型与多层扩散(DIF)模型。 DIF模型在根区域下面有或没有深层土层。通过在494-2010期间在45℃和48种草原荷泊尔比赛中使用法国农业统计,为45℃和48种草原荷泊尔定期进行分类的各种根水摄取模型的评价。模拟最大值 b ag 与梯度观察的显着相关性地用作标准,以基于基于根水uptakemodels的公制进行显着相关性。发现显着的相关性( p 值<0.01),分别为谷物和草原的129%和77%的Département。关于简化的土壤水文方案,发现了对最精致的MOSODEL的相当中性的影响。这表明应该在未来的研究中制定努力,以减少其他不确定性的其他来源,例如,通过使用更详细的土壤和根密度突发性与卫星植被产品一起使用。结果发现,额外的额外的副置区碱基流量土壤层不会改善(和部门甚至降解)The-Pround生物量的年间变异性的表示。这些结果特别强大的Forgrasslands,因为校准模拟能够分别代表与不利和有利的饲料生产相对应的极端2003和2007年。

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