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Exploration of parametric uncertainty in a surface mass balance model applied to the Greenland ice sheet

机译:探索应用于格陵兰冰盖的表面质量平衡模型中的参数不确定性

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Computational modeling of Earth system processes often requires simplifying assumptions of the real system. These necessary assumptions result in the definition of internal model parameters that can take a number of different values but must be explicitly defined for any one model simulation. The main issue with such an uncertain multidimensional input space is that many simulations are needed to adequately explore it. This study presents a generalized parameter screening experiment for use in future earth system modeling. This approach identifies model parameters that dominate uncertainty, therefore reducing to a manageable number the simulations required to explore the input space. The approach we adopt is relatively inexpensive to implement and can be applied at both the aggregate and disaggregate (e.g., regional) level. To demonstrate the potential of such a method, it is applied to a surface mass balance model of intermediate complexity over the Greenland ice sheet. All identified parameters were related to the surface melt parameterization, with albedo parameters being identified as the most important. Spatial distributions of the parameter sensitivities show that, in recent years, most parameter sensitivities are concentrated around the southwest and northern ice sheet margins. Simulations for the 21st century indicate an increase in sensitivity in these high melt areas especially in the northeast. Melt contributions from temperature and radiative effects are shown to be important on the order of parameters identified, and as a consequence, sensitivities are dependent on the present climate used for modeling surface mass balance.
机译:地球系统过程的计算建模通常需要简化实际系统的假设。这些必要的假设导致内部模型参数的定义可以采用许多不同的值,但必须为任何一个模型仿真明确定义。这种不确定的多维输入空间的主要问题是需要进行许多仿真才能充分探索它。这项研究提出了用于未来地球系统建模的广义参数筛选实验。这种方法可以识别主导不确定性的模型参数,从而将探索输入空间所需的仿真减少到可管理的数量。我们采用的方法实施起来相对便宜,并且可以在总体和细分(例如区域)级别应用。为了证明这种方法的潜力,将其应用于格陵兰冰原上中等复杂程度的表面质量平衡模型。所有确定的参数都与表面熔体参数化有关,其中反照率参数被认为是最重要的。参数敏感性的空间分布表明,近年来,大多数参数敏感性集中在西南和北部冰盖边缘附近。 21世纪的模拟表明,在这些高熔点地区,特别是东北地区,敏感性提高了。结果表明,温度和辐射效应对熔体的贡献在确定的参数顺序上很重要,因此,敏感性取决于用于模拟表面质量平衡的当前气候。

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