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Modelling DEM data uncertainties for Monte Carlo Simulations of Ice Sheet Models

机译:冰盖模型蒙特卡洛模拟的DEM数据不确定性建模

摘要

For realistic modelling of digital elevation model (DEM) uncertainty, information on the amount and spatial configuration is needed. However, common DEM products are often distributed with global error figures at best. Where no higher accuracy reference data is available, assumptions have to be made about the spatial distribution of uncertainty, that are often unrealistic. In order to assess the impact of DEM uncertainty on the results of an ice sheet model (ISM) for an area where no higher accuracy reference data was available, we quantified DEM error of comparable regions with available reference data. Deriving good correlation of error magnitude and spatial\udconfiguration with DEM characteristics, these dependencies were incorporated into an uncertainty model containing both deterministic and stochastic components. The developed uncertainty model proved to reproduce amount and spatial correlation of DEM error well while producing uncertainty surfaces suitable for Monte Carlo Simulations (MCS). Applying the model to a DEM of Fennoscandia, a MCS was conducted using an ISM during the first 40ka of the Last Glacial Maximum (LGM). Results showed DEM uncertainty to\udhave significant impact on model results during nucleation and retreat of the ice sheet.
机译:为了对数字高程模型(DEM)不确定性进行逼真的建模,需要有关数量和空间配置的信息。但是,常见的DEM产品通常最多都附带全局误差图。在没有更高准确度的参考数据可用的情况下,必须对不确定性的空间分布做出假设,这通常是不现实的。为了评估DEM不确定性对没有更高精度参考数据的区域的冰盖模型(ISM)结果的影响,我们使用可用参考数据对可比较区域的DEM误差进行了量化。得出误差大小和空间\ ud构型与DEM特征的良好相关性,将这些依赖性纳入包含确定性和随机性成分的不确定性模型中。事实证明,开发的不确定性模型可以很好地重现DEM误差的数量和空间相关性,同时生成适合于蒙特卡洛模拟(MCS)的不确定性表面。将模型应用于Fennoscandia的DEM,在最后一次冰期最大值(LGM)的前40ka期间,使用ISM进行了MCS。结果表明,DEM的不确定性会对冰盖成核和后退过程中的模型结果产生重大影响。

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