Difference between revisions of "Bathymetry"
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Dronkers J (talk | contribs) |
Dronkers J (talk | contribs) |
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− | The depths are | + | 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== | ||
+ | * [[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]] | + | * [[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
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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
- Satellite-derived nearshore bathymetry
- Use of X-band and HF radar in marine hydrography
- HyMap: Hyperspectral seafloor mapping and direct bathymetry calculation in littoral zones
References
- ↑ Lincoln R., Boxshall G. and Clark P. (1998). A Dictionary of Ecology, Evolution and Systematics (2nd Ed). Cambridge University Press: Cambridge, (England). 361pp.