首页> 外文期刊>Geoscientific Model Development >Autocalibration of a one-dimensional hydrodynamic-ecological model (DYRESM 4.0-CAEDYM 3.1) using a Monte Carlo approach: simulations of hypoxic events in a polymictic lake
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Autocalibration of a one-dimensional hydrodynamic-ecological model (DYRESM 4.0-CAEDYM 3.1) using a Monte Carlo approach: simulations of hypoxic events in a polymictic lake

机译:使用蒙特卡洛方法对一维水动力-生态模型(DYRESM 4.0-CAEDYM 3.1)进行自动校准:多聚湖泊中低氧事件的模拟

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Automated calibration of complex deterministic water quality models with a large number of biogeochemical parameters can reduce time-consuming iterative simulations involving empirical judgements of model fit. We undertook autocalibration of the one-dimensional hydrodynamic-ecological lake model DYRESM-CAEDYM, using a Monte Carlo sampling (MCS) method, in order to test the applicability of this procedure for shallow, polymictic Lake Rotorua (New Zealand). The calibration procedure involved independently minimizing the root-mean-square error (RMSE), maximizing the Pearson correlation coefficient (r) and Nash–Sutcliffe efficient coefficient (Nr) for comparisons of model state variables against measured data. An assigned number of parameter permutations was used for 10?000 simulation iterations. The "optimal" temperature calibration produced a RMSE of 0.54?°C, Nr value of 0.99, and r value of 0.98 through the whole water column based on comparisons with 540 observed water temperatures collected between 13?July?2007 and 13?January?2009. The modeled bottom dissolved oxygen concentration (20.5?m below surface) was compared with 467 available observations. The calculated RMSE of the simulations compared with the measurements was 1.78?mg?Lsup?1/sup, the Nr value was 0.75, and the r value was 0.87. The autocalibrated model was further tested for an independent data set by simulating bottom-water hypoxia events from 15 January 2009 to 8?June?2011 (875?days). This verification produced an accurate simulation of five hypoxic events corresponding to DO ?1/sup during summer of 2009–2011. The RMSE was 2.07?mg?Lsup?1/sup, Nr value 0.62, and r value of 0.81, based on the available data set of 738 days. The autocalibration software of DYRESM-CAEDYM developed here is substantially less time-consuming and more efficient in parameter optimization than traditional manual calibration which has been the standard tool practiced for similar complex water quality models.
机译:具有大量生物地球化学参数的复杂的确定性水质模型的自动校准可以减少涉及模型拟合的经验判断的耗时的迭代模拟。我们使用蒙特卡洛采样(MCS)方法对一维水动力-生态湖泊模型DYRESM-CAEDYM进行了自动校准,以测试该程序在浅层,多晶的罗托鲁瓦湖(新西兰)中的适用性。校准过程包括独立地最小化均方根误差(RMSE),最大化Pearson相关系数(r)和Nash-Sutcliffe有效系数(Nr),以比较模型状态变量与测量数据。分配了一定数量的参数置换用于10 000次仿真迭代。根据与2007年7月13日至2007年1月13日收集的540个观测水温的比较,“最佳”温度校准在整个水柱中的均方根误差为0.54?C,Nr值为0.99,r值为0.98。 2009年。将模拟的底部溶解氧浓度(表面以下20.5?m)与467个可用观测值进行了比较。与测量结果相比,模拟的RMSE值为1.78?mg?L ?1 ,Nr值为0.75,r值为0.87。通过模拟2009年1月15日至2011年6月8日(875天)的底水缺氧事件,进一步测试了自动校准模型的独立数据集。该验证对2009-2011年夏季对应于DO?1 的五个低氧事件进行了精确模拟。根据738天的可用数据集,RMSE为2.07?mg?L ?1 ,Nr值为0.62,r值为0.81。与传统的手动校准相比,此处开发的DYRESM-CAEDYM自动校准软件比传统的手动校准要少得多的时间和效率,而传统的手动校准已成为类似复杂水质模型的标准工具。

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