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Bathimetry Survey Basic Concept and Theory Overview

According to Poerbandono and Djunarsjah (2005), Bathymetry survey is a process and activity aimed at obtaining the seabed surface (model) surface shape (topography). The basic depiction of the waters (from measurement, processing to visualization) is referred to as bathymetry survey. The main purpose of bathymetry survey is safety of navigation. One method of measuring the depth of the ocean is by acoustic method (Figure below taken from http://www.ozcoasts.gov.au/glossary/def_s-t.jsp) using an echosounder. The echo device will produce an acoustic wave with a certain frequency that allows to penetrate a certain medium, in this case water. In the acoustic method the electrical energy is transformed into mechanical energy in the form of sound waves. Sound waves are emitted through the transducer, reflected by the seafloor and will be received back by the tranducer.
Principles calculations on the depth of the acoustic method is to calculate the time interval since the waves emitted and received back due to reflection by the bottom waters. The time interval is then multiplied by the velocity of acoustic waves in a water medium. The measurement results are displayed in the form of depth lines in the echogram and / or in digital form. Storage and appearance in digital form using navigation software capable of being integrated with measurement positions. Bathymetry survey begins with the manufacture of survey lines. The lanes are measured in depth and represented in the form of depth points. Each measured point has time, position, and depth variables. Position can be obtained by integrating echosounder with satellite navigation technology.
In bathymetry survey there are basic provisions that must be implemented. The provisions are made by the International Hydrographic Organization (IHO) published in the form of Special Publication Number 44 (SP-44 IHO) 5th Edition of 2008. The provisions in SP-44 IHO include:
IHO classifies the level of accuracy of surveys through the order. Determination of order based on topography of waters. Special Order is aimed at locations with marine waters that are hazardous to the safety of shipping, Order 1a is used for locations less than 100 m deep and less dangerous for shipping, Order 1b is used for locations less than 100 m deep and not harmful to safety cruises, and Order 2 for locations with a depth of more than 100 m.
The position of the measured depth points refers to the ITRF geocentric reference frame and preferably using WGS84. The confidence level of the position is determined at 95%. Each Order of accuracy survey has its own criteria in determining horizontal accuracy.
Depth value less than 200 m should be corrected against tidal. In addition, any object found during the survey and considered to interfere with the safety of shipping shall be reported to its position and depth.

Geophysical Surveying           Met-Ocean Survey

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