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The sensitivity and optimization of the model parameters for the simulation of latent heat flux

机译:潜热通量模拟的敏感性和模型参数的优化

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The land surface model (LSM) is very complex, and its parameters are one of the key sources of model prediction error. In order to improve the ability of the simulation, the study addressed the parameter sensitivity analysis, optimization and its effect on the simulated latent heat fluxes from the Noah LSM. The LH-OAT sensitivity analysis method was conducted for the Noah LSM to assess the sensitivity of model prediction of the latent heat flux to various model input parameters, the dominant vegetation and soil parameters were determined. Then, the model parameters are estimated from Noah LSM with a Bayesian framework by applying the Shuffled Complex evolution Metropolis Algorithm(SCEM-UA), an efficient Markov Chain Carlo sampler. The Noah model prediction using the optimal parameters shows that the LE simulated latent heat fluxes matched measurements fairly well with an R2 value of 0.9394, Root Mean Squared Error (RMSE) of 36.77W/m2, and mean bias error(MBE) of −1.17W/m2. Results demonstrate the ability of the combination LH-OAT method and the SCEM-UA algorithm for sensitivity analysis and parameter optimization in the Noah land surface model.
机译:地表模型(LSM)非常复杂,其参数是模型预测误差的关键来源之一。为了提高仿真能力,本研究针对参数灵敏度分析,优化及其对来自Noah LSM的仿真潜热通量的影响。对Noah LSM进行了LH-OAT敏感性分析方法,以评估潜热通量模型预测对各种模型输入参数的敏感性,确定了主要植被和土壤参数。然后,通过使用高效的马尔可夫链卡洛采样器Shuffled Complex Evolution Metropolis Algorithm(SCEM-UA),利用贝叶斯框架从Noah LSM估计模型参数。使用最佳参数进行的Noah模型预测表明,LE模拟的潜热通量与测量值匹配得很好,R 2 值为0.9394,均方根误差(RMSE)为36.77W / m2,均值偏置误差(MBE)为-1.17W / m 2 。结果表明,结合使用LH-OAT方法和SCEM-UA算法,可以在Noah地表模型中进行灵敏度分析和参数优化。

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