Comment on “High‐dimensional posterior exploration of hydrologic models using multiple‐try DREAM (ZS) and high‐performance computing” by Eric Laloy and Jasper A. Vrugt
Comment on “High‐dimensional posterior exploration of hydrologic models using multiple‐try DREAM (ZS) and high‐performance computing” by Eric Laloy and Jasper A. Vrugt
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DOI:
10.1002/2012wr013341
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发表时间:
2014-03
影响因子:
5.4
通讯作者:
Wei Chu;Tiantian Yang;Xiaogang Gao
中科院分区:
文献类型:
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作者:
Wei Chu;Tiantian Yang;Xiaogang Gao
Laloy and Vrugt [2012] (doi:10.1029/2011WR010608, hereafter referred to as LV) recently introduced a new Markov Chain Monte Carlo (MCMC) algorithm, entitled MT-DREAM(ZS). To illustrate the improved performance of this new algorithm, LV compared it against another adaptive MCMC approach, DREAM(ZS) [Vrugt et al., 2009], and a direct search method, SP-UCI [Chu et al., 2010]. The modeling cases used as benchmarks were the Sacramento Soil Moisture Accounting (SAC-SMA) model and a 241-parameter groundwater model developed by Keating et al. [2010]. Based on their experimental results, LV concludes that ‘‘SP-UCI performs poorly’’ on both models, therefore LV raises the question about the ability of SP-UCI to deal with complex and multimodal searching spaces. Also, the experiments show that MT-DREAM algorithm demonstrates substantial improvement over DREAM(ZS) and SP-UCI for searching the global optima of high-dimensional models. We congratulate LV on their new algorithm and the consistent performances for the test examples provided in the MT-DREAM(ZS) and DREAM(ZS) packages. However, after repeating other two conclusive experiments in LV’s paper, we would like to communicate our concerns regarding the unfair judgments about the performance and ability of SP-UCI for these two models. Also, we are puzzled about the reproducibility of the experimental results and the effectiveness of the MT-DREAM(ZS) algorithm in assessing complex posterior distributions reported by LV about both the MT-DREAM and SP-UCI algorithms on the SACSMA model and the 241-parameter ground water model.