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Exploring uncertainty in glacier mass balance modelling with Monte Carlo simulation

机译:利用蒙特卡洛模拟探索冰川质量平衡模型的不确定性

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摘要

By means of Monte Carlo simulations we calculated uncertainty in modelled cumulative mass balance over 400 days at one particular point on the tongue of Morteratsch Glacier, Switzerland, using a glacier energy balance model of intermediate complexity. Before uncertainty assessment, the model was tuned to observed mass balance for the investigated time period and its robustness was tested by comparing observed and modelled mass balance over 11 years, yielding very small deviations. Both systematic and random uncertainties are assigned to twelve input parameters and their respective values estimated from the literature or from available meteorological data sets. The calculated overall uncertainty in the model output is dominated by systematic errors and amounts to 0.7 m w.e. or approximately 10% of total melt over the investigated time span. In order to provide a first order estimate on variability in uncertainty depending on the quality of input data, we conducted a further experiment, calculating overall uncertainty for different levels of uncertainty in measured global radiation and air temperature. Our results show that the output of a well calibrated model is subject to considerable uncertainties, in particular when applied for extrapolation in time and space where systematic errors are likely to be an important issue.
机译:通过蒙特卡洛模拟,我们使用中等复杂程度的冰川能量平衡模型,计算了瑞士Morteratsch冰川舌头上某一特定点在400天内累积质量平衡模型的不确定性。在进行不确定性评估之前,将模型调整为所调查时间段内的观察到的质量平衡,并通过比较11年内观察到的和建模的质量平衡来测试其健壮性,从而产生很小的偏差。系统性不确定性和随机性不确定性都分配给了十二个输入参数,它们各自的值是从文献或从可用的气象数据集中估算出来的。在模型输出中计算出的总体不确定性受系统误差支配,总计0.7 m w.e.或在研究的时间范围内约占总熔体的10%。为了对不确定性的可变性(取决于输入数据的质量)提供一阶估计,我们进行了进一步的实验,针对测得的全球辐射和气温的不同不确定性水平,计算了总体不确定性。我们的结果表明,经过良好校准的模型的输出会受到相当大的不确定性影响,尤其是在将时间和空间应用于系统误差可能是重要问题的外推法时。

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