2015
DOI: 10.1016/j.envsoft.2015.02.007
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Selecting model scenarios of real hydrodynamic forcings on mesotidal and macrotidal estuaries influenced by river discharges using K-means clustering

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Cited by 24 publications
(12 citation statements)
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“…As a result, a preliminary study embraces all possible plume patterns is necessary, and a first step is to target the general behavior of the estuarine-plume system. Bárcena et al, (2015) explained that two approaches may be conducted for that: simulating several scenarios using constant conditions of hydrodynamic forcings or simulating few scenarios using the most frequent or extreme real hydrodynamic forcings during short-medium term periods (month to year).…”
Section: J O U R N a L P R E -P R O O Fmentioning
confidence: 99%
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“…As a result, a preliminary study embraces all possible plume patterns is necessary, and a first step is to target the general behavior of the estuarine-plume system. Bárcena et al, (2015) explained that two approaches may be conducted for that: simulating several scenarios using constant conditions of hydrodynamic forcings or simulating few scenarios using the most frequent or extreme real hydrodynamic forcings during short-medium term periods (month to year).…”
Section: J O U R N a L P R E -P R O O Fmentioning
confidence: 99%
“…Also, without any prior information on the cluster structure (sphericity of clusters, possible overlap) the fuzzy c-mean provides better results than its crisp counterpart (Selim & Kamel, 1992). As a result, hydrologic and climatologic combinations can be identified by fuzzy-cmean (Kim et al, 2011;Zhang et al, 2011;Bárcena et al, 2015).…”
Section: Fuzzy C-mean Algorithmmentioning
confidence: 99%
“…A comparison between the original tide series and the synthetic time series reconstructed with the clusters derived from these classifications was performed using the efficiency coefficient (CE). CE was selected because it is the best objective function for reflecting the overall adjustment of a clustering output (Bárcena et al., 2015). CE is a normalized statistic developed by Nash and Sutcliffe (1970) that determines the relative magnitude of the residual variance ( noise ) and therefore reflects the accuracy with which the centroids estimate the original data (Equation ): CE=true1nfalse(OiCifalse)2true1nfalse(OiŌfalse)2, where O i is the i‐data ( γ 1 , g 2 , or TR) of the original series, C i is the i‐data ( γ 1 , g 2 , or TR) of the representative centroid and n is the number of nodes where the tide is evaluated.…”
Section: Statistical and Cluster Analysis Of Global Tide Asymmetrymentioning
confidence: 99%
“…In the first step, the k-means algorithm was used to partition the changed land use cells during T1 to T2 into five clusters. The k-means clustering technique is capable of dividing multidimensional data into a number of clusters by defining prototypes and calculating the distance to each prototype (Bárcena et al 2015). It is commonly used to automatically partition a data set into k groups by selecting k initial cluster centers and then iteratively refining them as follows:…”
Section: Partitioning the Research Area By K-means And Knn-cluster Almentioning
confidence: 99%