Difference between revisions of "Bathymetry"

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The depths are almost always derived indirectly by measuring the time required for a signal to travel from a transmitter, to the bottom, and back to a receiver.
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The depths are generally derived indirectly by measuring the time required for a signal to travel from a transmitter, to the bottom, and back to a receiver.
  
  
 
==See also==
 
==See also==
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* [[Satellite-derived nearshore bathymetry]]
 
* [[Use of X-band and HF radar in marine hydrography]]
 
* [[Use of X-band and HF radar in marine hydrography]]
* [[Hyperspectral seafloor mapping and direct bathymetry calculation in littoral zones]]
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* [[HyMap: Hyperspectral seafloor mapping and direct bathymetry calculation in littoral zones]]
  
 
==References==
 
==References==
 
<references/>
 
<references/>

Latest revision as of 12:14, 7 December 2023

Definition of Bathymetry:
Mapping of the seafloor depth with respect to the mean water level and the study of floor topography (Lincoln & Boxshall, 1987).[1].
This is the common definition for Bathymetry, other definitions can be discussed in the article


The depths are generally derived indirectly by measuring the time required for a signal to travel from a transmitter, to the bottom, and back to a receiver.


See also

References

  1. Lincoln R., Boxshall G. and Clark P. (1998). A Dictionary of Ecology, Evolution and Systematics (2nd Ed). Cambridge University Press: Cambridge, (England). 361pp.