XXII ISPRS Congress 2012: Technical Commission VIII

Shortis, M.; Shimoda, H.; Cho, K.

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Multivolume work

Persistent identifier:: 1663813779

Title:: XXII ISPRS Congress 2012

Sub title:: Melbourne, Australia, 25 August-1 September 2012

Year of publication:: 2013

Place of publication:: Red Hook, NY

Publisher of the original:: Curran Associates, Inc.

Identifier (digital):: 1663813779

Language:: English

Additional Notes:: Kongress-Thema: Imaging a sustainable future

Corporations:: International Society for Photogrammetry and Remote Sensing, Congress, 22., 2012, Melbourne; International Society for Photogrammetry and Remote Sensing

Adapter:: International Society for Photogrammetry and Remote Sensing, Congress, 22., 2012, Melbourne; International Society for Photogrammetry and Remote Sensing

Founder of work:: International Society for Photogrammetry and Remote Sensing, Congress, 22., 2012, Melbourne; International Society for Photogrammetry and Remote Sensing

Other corporate:: International Society for Photogrammetry and Remote Sensing, Congress, 22., 2012, Melbourne; International Society for Photogrammetry and Remote Sensing

Document type:: Multivolume work

Volume

Persistent identifier:: 1663822514

Title:: Technical Commission VIII

Scope:: 590 Seiten

Year of publication:: 2014

Place of publication:: Red Hook, NY

Publisher of the original:: Curran Associates, Inc.

Identifier (digital):: 1663822514

Illustration:: Illustrationen, Diagramme

Signature of the source:: ZS 312(39,B8)

Language:: English

Additional Notes:: Erscheinungsdatum des Originals ist ermittelt.; Literaturangaben

Usage licence:: Attribution 4.0 International (CC BY 4.0)

Editor:: Shortis, M.; Shimoda, H.; Cho, K.

Corporations:: International Society for Photogrammetry and Remote Sensing, Congress, 22., 2012, Melbourne; International Society for Photogrammetry and Remote Sensing

Adapter:: International Society for Photogrammetry and Remote Sensing, Congress, 22., 2012, Melbourne; International Society for Photogrammetry and Remote Sensing

Founder of work:: International Society for Photogrammetry and Remote Sensing, Congress, 22., 2012, Melbourne; International Society for Photogrammetry and Remote Sensing

Other corporate:: International Society for Photogrammetry and Remote Sensing, Congress, 22., 2012, Melbourne; International Society for Photogrammetry and Remote Sensing

Publisher of the digital copy:: Technische Informationsbibliothek Hannover

Place of publication of the digital copy:: Hannover

Year of publication of the original:: 2019

Document type:: Volume

Collection:: Earth sciences

Chapter

Title:: [VIII/4: Water]

Document type:: Multivolume work

Structure type:: Chapter

Chapter

Title:: COASTAL CURRENTS MONITORING USING RADAR SATELLITES BASED ON WAVE TRACKING APPROACH A. Abedini, M. Aghamohamadnia, M. Sharifi, S. Farzaneh

Document type:: Multivolume work

Structure type:: Chapter

38, 2012 dimensional below Eql tem in the )e easier to | way which precision be ion and also rithm below ; limit range Q) hood of shape like a ; considered > edges are ond surface | for normal ne, which is is located in er surface is . of volume ons on the low (Fig3). momentum of a plane omentum of e impact of respectively. International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences, Volume XXXIX-B8, 2012 XXII ISPRS Congress, 25 August — 01 September 2012, Melbourne, Australia The second row figures show a similar cross section of surface but indicate the relative location of both first and second order of momentums to be used in direction finding procedure. It is obvious that both orders points in the normal shape are coincident while there is a displacement of both of them in the inclined and affected state. The vector connecting first to second order point introduces the inclination direction of wave's peak in a 3 dimensional space. Portraying this vector on the X-Y plane gives the direction of the current in the local coordinate system, which will be transferred in the specific coordinate system for further use. Here are the equations to compute the first and second order surface momentum having the coordinates of points Eq3. em ym d Wired Direc Lun 3 Figure 3. a) First order of surface momentum point of resulted surface of a normal wave in a cross section of a plane perpendicular to the X-Y plane (Most top). b) Distance vector between surface points and First order of surface momentum point of resulted surface of a deformed wave in a cross section of a plane perpendicular to the X-Y plane (Top). c) Second order of surface momentum point of resulted surface of a normal wave in a cross section of a plane perpendicular to the X-Y plane (Lower). d) First and Second order of surface momentum point of resulted surface of a deformed wave in a cross section of a plane perpendicular to the X-Y plane (bottom). G) Where r(i) Distance between the first momentum and surface Points O(k) First surface momentum point of kth maximum point O’(k) Second surface momentum point of kth maximum point P(i) The ith point of surface peak The second order surface momentum inclines toward the sharpness tip of a deformed shape. Finally to get a better and more reliable result out of this method, the surface model can be accompanied with the bathymetric models of the area. 3. THE DATA USED AND RESULTS The method described above must be applied on a dataset in order to see its impact and results in a real case. For some reasons the TerraSAR-X dataset was not accessible and we were obliged to use another satellite data. The data used in this paper is from Jason] satellite altimeter and was taken from the NOAA (4| website. Hope to use the TerraSAR-X data in the future works. The Surface model is determined using the Delaunay triangulation method. This surface has been used in our method and the results which were in the local datum have been transferred in to the UTM system. For better demonstration and use of dataset results, the vector field has been exported in the KML format to be shown in the Google Earth Environment. The location of data set is over the Hormuz strait connecting The Persian Gulf and The Oman Sea. Vector field over the Hormuz Strait is shown in the Figures (4, 5 and 6). Figure 4. Surface current vector field Over the Coastal area of Hormuz Strait in an overall view and low resolution but high density. Figure 5. Surface current vector field Over the Coastal area of Hormuz Strait in detailed view and high resolution and vector density.

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