K nearest neighbors classification of water masses in the western Alboran Sea using the sigma-pi diagram

被引:5
作者
Belattmania, Ayoub [1 ]
El Arrim, Abdelkrim [1 ]
Ayouche, Adam [2 ]
Charria, Guillaume [2 ]
Hilmi, Karim [3 ]
El Moumni, Bouchta [4 ]
机构
[1] Fac Sci Tech, Tanger, Morocco
[2] Univ Brest, Lab Ocean Phys & Satell Remote Sensing LOPS, UMR6523, Ifremer,CNRS,IRD, Brest, France
[3] Inst Natl Rech Halieut, Casablanca, Morocco
[4] Univ Abdelmalek Essaadi, Tetouan, Morocco
关键词
Alboran sea; Western Alboran Gyre; Water masses; (& sigma; -& pi; ) diagram; K nearest neighbor classification; FREQUENCY DISTRIBUTION; CIRCULATION; MIGRATION; DEEP;
D O I
10.1016/j.dsr.2023.104024
中图分类号
P7 [海洋学];
学科分类号
0707 ;
摘要
Different classification techniques of water masses have been developped using the potential temperature-salinity (?-S) diagram and its volumetric analysis. In this study, we propose a new method to automatically classify water masses via a supervised machine learning algorithm based on the K nearest neighbors (Knn), in the potential density and potential spicity (s-p) coordinates. This method is applied to temperature and salinity data collected in the western side of the Alboran Sea during a glider mission, dedicated to sample the Western Alboran Gyre (WAG) in late winter 2021. The water masses in the studied region were classified into five different categories following a supervised learning process, based on ocean profile databases available on the region of interest. The results corroborate previous studies of the spatial distribution of water masses in the Alboran Sea, inferred from traditional method based on the expert analysis of the (?-S) diagram, and suggest that this methodology is efficient and reliable for water masses classification. Compared to a classical clustering computation (herein k-means), this method is more appropriate in a region where the characteristics of the water masses change considerably in both space and time.
引用
收藏
页数:26
相关论文
共 62 条
[1]  
Akhir M.F., 2015, OPEN J MAR SCI, V5, P273, DOI [DOI 10.4236/ojms.2015.54036, 10.4236/ojms.2015.54036]
[2]  
Ambarwari A., 2020, J. RESTI, V4, P117, DOI DOI 10.29207/RESTI.V4I1.1517
[3]  
Argo, 2000, Argo Data Sources
[4]   Spreading of Levantine Intermediate Waters by submesoscale coherent vortices in the northwestern Mediterranean Sea as observed with gliders [J].
Bosse, Anthony ;
Testor, Pierre ;
Mortier, Laurent ;
Prieur, Louis ;
Taillandier, Vincent ;
d'Ortenzio, Fabrizio ;
Coppola, Laurent .
JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, 2015, 120 (03) :1599-1622
[5]  
Boyer T.P., 2018, WORLD OCEAN DATABASE, DOI DOI 10.13140/RG.2.2.34758.01602
[6]  
Broecker W. S., 1991, Oceanography, V4, P79, DOI DOI 10.5670/OCEANOG.1991.07
[7]  
Bryden H.L, 1982, ORIGIN MEDITERRANEAN
[8]   Fast neighbor search by using revised k-d tree [J].
Chen, Yewang ;
Zhou, Lida ;
Tang, Yi ;
Singh, Jai Puneet ;
Bouguila, Nizar ;
Wang, Cheng ;
Wang, Huazhen ;
Du, Jixiang .
INFORMATION SCIENCES, 2019, 472 :145-162
[9]  
Cheng Guo-sheng, 2014, Journal of Tropical Oceanography, V33, P10, DOI 10.3969/j.issn.1009-5470.2014.03.002
[10]   The role of the thermohaline circulation in abrupt climate change [J].
Clark, PU ;
Pisias, NG ;
Stocker, TF ;
Weaver, AJ .
NATURE, 2002, 415 (6874) :863-869