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首页> 外文期刊>Geoscientific Model Development Discussions >An iterative process for efficient optimisation of parameters in geoscientific models: a demonstration using the Parallel Ice Sheet Model (PISM) version 0.7.3
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An iterative process for efficient optimisation of parameters in geoscientific models: a demonstration using the Parallel Ice Sheet Model (PISM) version 0.7.3

机译:高效优化地球科学型号参数优化的迭代过程:使用并行冰板模型(Pism)版本0.7.3

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Physical processes within geoscientific models are sometimes described by simplified schemes known as parameterisations. The values of the parameters within these schemes can be poorly constrained by theory or observation. Uncertainty in the parameter values translates into uncertainty in the outputs of the models. Proper quantification of the uncertainty in model predictions therefore requires a systematic approach for sampling parameter space. In this study, we develop a simple and efficient approach to identify regions of multi-dimensional parameter space that are consistent with observations. Using the Parallel Ice Sheet Model to simulate the present-day state of the Antarctic Ice Sheet, we find that co-dependencies between parameters preclude any simple identification of a single optimal set of parameter values. Approaches such as large ensemble modelling are therefore required in order to generate model predictions that incorporate proper quantification of the uncertainty arising from the parameterisation of physical processes.
机译:有时通过称为参数化的简化方案来描述地质模型中的物理过程。这些方案中的参数的值可能因理论或观察而受到严重限制。参数值中的不确定性转化为模型输出中的不确定性。因此,适当地定量模型预测中的不确定性需要一种用于采样参数空间的系统方法。在这项研究中,我们开发了一种简单有效的方法来识别与观察结果一致的多维参数空间区域。使用并行冰板模型来模拟南极冰盖的当代状态,我们发现参数之间的共同依赖性排除了任何简单的识别单个最佳参数值。因此,需要诸如大型集合建模的方法,以便生成含有从物理过程的参数化引起的不确定性的适当量化的模型预测。

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