Application of multivariate statistical techniques in alongshore differentiation of coastal barriers

被引:12
作者
Borges Bitencourt, Volney Junior [1 ]
Dillenburg, Sergio R. [2 ]
机构
[1] Univ Fed Rio Grande do Sul, Inst Geociencias, Programa Posgrad Geociencias, Av Bento Goncalves 9500, BR-91509900 Porto Alegre, RS, Brazil
[2] Univ Fed Rio Grande do Sul, Ctr Estudos Geol Costeira & Ocean, Inst Geociencias, Av Bento Goncalves 9500, BR-91509900 Porto Alegre, RS, Brazil
关键词
Coastal evolution; Beach morphodynamics; Principal Component Analysis (PCA); Hierarchical Cluster Analysis (HCA); GRANDE-DO-SUL; SEA-LEVEL RISE; PRINCIPAL COMPONENT ANALYSIS; LATE-HOLOCENE; SEDIMENT TRANSPORT; SOUTHERN BRAZIL; WAVE-ENERGY; TRANSGRESSIVE DUNEFIELDS; BEACH MORPHODYNAMICS; ACCOMMODATION SPACE;
D O I
10.1016/j.margeo.2019.106077
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
This paper investigates the existence of statistical correlations and relationships between geological and oceanographic parameters along a coastal barrier system in southern Brazil. The existence of few statistical studies on coastal barriers motivated the use of multivariate statistical techniques that take environmental parameters such as coastal morphological-sedimentary features and their morphometric measurements into account. The Hierarchical Cluster Analysis (HCA) and Principal Component Analysis (PCA) were used to assess the spatial variations of fourteen parameters driving the current and past behavior of this coastal barrier system at fourteen locations. Through the application of HCA, these locations were divided into four groups (Groups 1, 2, 3, and 4). The HCA results were analyzed using PCA. The first (PC1) and the second (PC2) principal components together explained at least 76.4% of the variability of all four groups. The most important geological and oceanographic parameters that were correlated to PC1 and PC2 were different in each group. In general, the shoreface slope and shoreface dimensions were common to all groups as PC1-correlated parameters, being the most important ones regarding data variability. In addition, for the progradational (Groups 1 and 4), retrogradational (Group 2) and aggradational barriers (Group 3) PCA indicated that shoreline orientation (wave exposure) and beach type are secondary, but relevant factors controlling the past and current behavior of coastal barriers in southern Brazil.
引用
收藏
页数:14
相关论文
共 154 条
[1]   Sediment supply from shoreface to dunes: linking sediment transport measurements and long-term morphological evolution [J].
Aagaard, T ;
Davidson-Arnott, R ;
Greenwood, B ;
Nielsen, J .
GEOMORPHOLOGY, 2004, 60 (1-2) :205-224
[2]   Principal component analysis [J].
Abdi, Herve ;
Williams, Lynne J. .
WILEY INTERDISCIPLINARY REVIEWS-COMPUTATIONAL STATISTICS, 2010, 2 (04) :433-459
[3]   Sedimentation processes and beach morphodynamics active at the Doce River mouth, Espirito Santo State, Brazil [J].
Albino, Jacqueline ;
Suguio, Kenitiro .
ANAIS DA ACADEMIA BRASILEIRA DE CIENCIAS, 2010, 82 (04) :1031-1044
[4]   Thresholds for morphological changes on an exposed sandy beach as a function of wave height [J].
Almeida, L. P. ;
Ferreira, O. ;
Pacheco, A. .
EARTH SURFACE PROCESSES AND LANDFORMS, 2011, 36 (04) :523-532
[5]   Koppen's climate classification map for Brazil [J].
Alvares, Clayton Alcarde ;
Stape, Jose Luiz ;
Sentelhas, Paulo Cesar ;
de Moraes Goncalves, Jose Leonardo ;
Sparovek, Gerd .
METEOROLOGISCHE ZEITSCHRIFT, 2013, 22 (06) :711-728
[6]  
Andrade MM, 2018, BRAZ J OCEANOGR, V66, DOI [10.1590/S1679-87592018017406603, 10.1590/s1679-87592018017406603]
[7]   A critical review of mid- to late-Holocene sea-level fluctuations on the eastern Brazilian coastline [J].
Angulo, RJ ;
Lessa, GC ;
de Souza, MC .
QUATERNARY SCIENCE REVIEWS, 2006, 25 (5-6) :486-506
[8]  
Angulo RJ, 2009, LECT NOTES EARTH SCI, V107, P135
[9]  
[Anonymous], 2010, J AQUATIC SCI
[10]  
[Anonymous], 2006, Erosao e progradacao do litoral brasileiro