Sensitivity analysis on a multilayer perceptron model for recognizing liquefaction cases     

Chung-Jung Lee  Ta-Kang Hsiung 《Computers and Geotechnics》2009,36(7):1157-1163

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基于引力模型的海洋锋信息提取   总被引：2，自引：0，他引：2  

平博  苏奋振  杜云艳  孟云闪  苏伟光 《地球信息科学学报》2013,15(2):187-192

海洋锋面是海洋水团特性明显不同的两种或几种水体之间的狭窄过渡带。本文旨在对遥感反演海洋温度场数据(SST),引入引力模型进行海洋锋面的检测。鉴于海洋锋受噪声干扰大,锋面强度小的特点,本文提出了基于引力算法的引力模型。其中,引力算法是将温度数据中的每一个像元点都作为一个独立的天体,其质量对应该像元的温度值,根据引力定律计算3×3区域中,邻域像元对中心点像元的引力和。模型首先对原始数据进行去0处理,为消除对原始数据明暗程度的依赖,对3×3区域数据进行归一化,然后利用函数对归一化后的数据进行增强处理,最后,以引力算法进行锋面检测。验证表明,该模型能有效强化不同区域或水体差异性,并能够有效针对海洋锋信息进行提取,受噪声影响小。  相似文献   

The study on three-dimensional numerical model and fronts of the Jiulong Estuary and the Xiamen Bay   总被引：1，自引：1，他引：0  

LUO Zhibin  PAN Weiran  LI Li  ZHANG Guorong 《海洋学报(英文版)》2012,31(4):55-64

Applying the methods of on-site observation and dynamic model, the research on the fronts at the Jiulong Estuary has been carried out, during which spatial and temporal distribution, dynamic characteristics and formation mechanism of salinity fronts are analyzed and discussed. The research shows that the estuarine fronts mainly lie in the area from the Jiyu Islet to the Haimen Island, outside of Yuweizai to Hulishan cross-section, the near coast of Yuweizai and the south of the Songyu-Gulangyu Channel. The fronts in the former two regions are formed directly by plume, while the one near the coast of Yuweizai is a tidal intrusion front caused by flood current and the one at the south of the Songyu-Gulangyu Channel is the result of current shear transformation. Under normal circumstances, fresh water of the Jiulong River mainly influences the inside of the Xiamen Bay, and when it is in typhoon seasons, plume front can affect the Taiwan Strait and has an effect on the biogeochemical processes in the strait.  相似文献   

A soil water and heat transfer model including changes in soil frost and thaw fronts     

WANG AiWen  XIE ZhengHui  FENG XiaoBing  TIAN XiangJun  QIN PeiHua 《中国科学:地球科学(英文版)》2014,57(6):1325-1339

Freeze-thaw processes in soils,including changes in frost and thaw fronts(FTFs),are important physical processes.The movement of FTFs affects soil hydrothermal characteristics,as well as energy and water exchanges between the land surface and the atmosphere and hydrothermal processes in the land surface.This paper reduces the issue of soil freezing and thawing to a multiple moving-boundary problem and develops a soil water and heat transfer model which considers the effects of FTF on soil hydrothermal processes.A local adaptive variable-grid method is used to discretize the model.Sensitivity tests based on the hierarchical structure of the Community Land Model(CLM)show that multiple FTFs can be continuously tracked,which overcomes the difficulties of isotherms that cannot simultaneously simulate multiple FTFs in the same soil layer.The local adaptive variable-grid method is stable and offers computational efficiency several times greater than the high-resolution case.The simulated FTF depths,soil temperatures,and soil moisture values fit well with the observed data,which further demonstrates the potential application of this simulation to the land-surface process model.  相似文献   

多层次跟踪预报法在地下流体会商中的应用     

张清秀  陈小云  薛飞 《福建地震》2005,(Z1)

本文介绍利用多层次跟踪预报方法之短期预测法在多次福建地下流体资料会商中的应用。水化多层次跟踪预报方法以“水化的多层次跟踪加速前兆图象”为依据进行分析,主要对地震的发震时间进行预测。该图象说明了水化的异常群体随时间的演变趋势与地震活动有关;异常群体的演变与地震之间具有“增长———地震”或“加速———地震”的关系。这种关系,同彭德银等指出的地震总是处于接近或偏离临界状态的演化进程中的理论相适应。  相似文献   

Comparative study of multilayer perceptron-stochastic gradient descent and gradient boosted trees for predicting daily suspended sediment load: The case study of the Mississippi River,U.S.     

Sadra Shadkani  Akram Abbaspour  Saeed Samadianfard  Sajjad Hashemi  Amirhosein Mosavi  Shahab S.Band 《国际泥沙研究》2021,36(4):512-523

Monitoring sediment transport is essential for managing and maintaining rivers.Estimation of the sediment load in rivers is fundamental for the study of sediment movement,erosion,and flood control.In the current study,three machine learning models-multi-layer perceptron(MLP),multi-layer perceptron-stochastic gradient descent(MLP-SGD),and gradient boosted tree(GBT)-were utilized to estimate the suspended sediment load(SSL)at the St.Louis(SL)and Chester(CH)stations on the Mississippi River,U.S.Four evaluation criteria including the Correlation Coefficient(CC),Nash Sutcliffe Efficiency(NSE),Scatter Index(SI),and Willmott’s Index(WI)were utilized to evaluate the performance of the used models.A sensitivity analysis of the models to the input variables revealed that the current day discharge variable had the most effect on the SSL at both stations,but in the absence of current-day discharge data(Qt),a combination of input parameters including SSL_t-3,SSL_t-2,SSL_t-1,Q_t-3,Q_t-2,Q_t-1 can be used to estimate the SSL.The comparative outcomes indicated the high accuracy of MLP-SGD-5 model with a CC of 0.983,SI of 0.254,WI of 0.991,and NSE of 0.967 at station CH and the MLP-SGD-6 model with a CC of 0.933,SI of 0.576,WI of 0.961,and NSE of 0.867,respectively,at station SL.The results of MLP models were improved by SGD optimization.Therefore,the MLP-SGD method is recommended as the most accurate model for SSL estimation.  相似文献   

用地下水位异常对1998年1月10日张北-尚义M_S6.2地震的检验性预测          下载免费PDF全文

高立新  曹刚 《地震工程学报》1999,21(3):334-336

分析了１９９８ 年１ 月１０ 日张北尚义 Ｍ Ｓ６ ．２ 地震前后晋冀蒙交界地区前兆台网地下水位异常特征．用多层次跟踪预报法对该次地震进行了检验性预测,探讨了地下水位高值异常与该次地震的关系．检验预测结果表明,这些异常就是该次地震的前兆反映  相似文献