期刊文献+

Application of Active Contour Model in Tracking Sequential Nearshore Waves

Application of Active Contour Model in Tracking Sequential Nearshore Waves
下载PDF
导出
摘要 In the present study, a generalized active contour model of gradient vector flow is combined with the video techniques of Argus system to delineate and track sequential nearshore wave crest profiles in the shoaling process, up to their breaking on the shoreline. Previous applications of active contour models to water wave problems are limited to controllable wave tank experiments. By contrast, our application in this study is in a nearshore field environment where oblique images obtained under natural and varying condition of ambient light are employed. Existing Argus techniques produce plane image data or time series data from a selected small subset of discrete pixels. By contrast, the active contour model produces line image data along continuous visible curves such as wave crest profiles. The combination of these two existing techniques, the active contour model and Argus methodologies, facilitates the estimates of the direction wave field and phase speeds within the whole area covered by camera. These estimates are useful for the purpose of inverse calculation of the water depth. Applications of the present techniques to Hsi-tzu bay where a beach restoration program is currently undertaken are illustrated. This extension of Argus video techniques provides new application of optical remote sensing to study the hydrodynamics and morphology of a nearshore environment. In the present study, a generalized active contour model of gradient vector flow is combined with the video techniques of Argus system to delineate and track sequential nearshore wave crest profiles in the shoaling process, up to their breaking on the shoreline. Previous applications of active contour models to water wave problems are limited to controllable wave tank experiments. By contrast, our application in this study is in a nearshore field environment where oblique images obtained under natural and varying condition of ambient light are employed. Existing Argus techniques produce plane image data or time series data from a selected small subset of discrete pixels. By contrast, the active contour model produces line image data along continuous visible curves such as wave crest profiles. The combination of these two existing techniques, the active contour model and Argus methodologies, facilitates the estimates of the direction wave field and phase speeds within the whole area covered by camera. These estimates are useful for the purpose of inverse calculation of the water depth. Applications of the present techniques to Hsi-tzu bay where a beach restoration program is currently undertaken are illustrated. This extension of Argus video techniques provides new application of optical remote sensing to study the hydrodynamics and morphology of a nearshore environment.
出处 《China Ocean Engineering》 SCIE EI 2009年第2期251-266,共16页 中国海洋工程(英文版)
基金 supported by the Science Council,Taiwan,under Grant No.NSC95-2221-E-006-475-MY2
关键词 active contour model SNAKE video images NEARSHORE active contour model snake video images nearshore
  • 相关文献

参考文献28

  • 1Aarninkhof,S.G.,Ruessink,B.G.and Roelvink,J.A.,2005.Nearshore subtidal bathymetry from time-exposure video images,Journal of Geophysical Research,110(C6):1-13.
  • 2Abdel-Aziz,Y.I.and Karara,H.M.,1971.Direct linear transformation from comparator coordinates into object space coordinates in close-range photogrammetry,Proceedings of the Symposium on Close-Range Photogrammetry,Urgana,IL.,1-18.
  • 3Alexander,P.S.and Holman,R.A.,2004.Quantification of nearshore morphology based on video imaging,Marine Geology,208(1):101-111.
  • 4Benetazzo,A.,2006.Measurements of short water waves using stereo matched image sequences,Coast.Eng.,53(12):1013-1032.
  • 5Duncan J.H.,Qiao,H.,Philomin,V.and Wenz,A.,1999.Gentle spilling breakers:crest profile evolution,J.Fluid Mech.,379,191 -222.
  • 6Holland K.T.,Raubenheimer,B.,Guza,R.T.and Holman,R.A.,1995.Runup kinematics on a natural beach,Journal of Geophysical Research,100(C3):4985-4993.
  • 7Holland.K.T.and Holman,R.A.,1996.Field observations of beach cusps and swash motions,Marine Geology,134(1-2):77-93.
  • 8Holland.K.T.and Holman,R.A.,1997.Video estimation of foreshore topography using trinocular stereo,Journal of Coastal Research,13(1):81-87.
  • 9Holland.K.T.,Holman,R.A.,Lippmann,T.C.,Stanley,J.and Plant,N.,1997.Practical use of vidoo imagery in nearshore oceanographic field studies,IEEE J.Ocean.Eng.,22(1):81-92.
  • 10Holman R.A.and Guza,R.T.,1984.Measuring run-up on a natural beach,Coast.Eng.,8(2):129-140.

相关作者

内容加载中请稍等...

相关机构

内容加载中请稍等...

相关主题

内容加载中请稍等...

浏览历史

内容加载中请稍等...
;
使用帮助 返回顶部