Bathymetry (pronounced ) is the study of underwater depth of ocean floor
s or lake floor
s. In other words, bathymetry is the underwater equivalent to hypsometry
. The name comes from Greek
βαθύς (''bathus''), "deep", and μέτρον (''metron''), "measure". Bathymetric (or hydrographic
) charts are typically produced to support safety of surface or sub-surface navigation, and usually show seafloor relief or terrain
as contour lines
(called depth contours or isobaths) and selected depths (soundings), and typically also provide surface navigation
al information. Bathymetric maps (a more general term where navigational safety is not a concern) may also use a Digital Terrain Model
and artificial illumination techniques to illustrate the depths being portrayed. The global bathymetry is sometimes combined with topography data to yield a Global Relief Model
. Paleobathymetry is the study of past underwater depths.
Originally, bathymetry involved the measurement of ocean
depth through depth sounding
. Early techniques used pre-measured heavy rope
or cable lowered over a ship's side.
This technique measures the depth only a singular point at a time, and is therefore inefficient. It is also subject to movements of the ship and currents moving the line out of true and therefore is not accurate.
The data used to make bathymetric maps today typically comes from an echosounder (sonar
) mounted beneath or over the side of a boat, "pinging" a beam of sound downward at the seafloor or from remote sensing LIDAR
or LADAR systems.
The amount of time it takes for the sound or light to travel through the water, bounce off the seafloor, and return to the sounder informs the equipment of the distance to the seafloor. LIDAR/LADAR surveys are usually conducted by airborne systems.
Starting in the early 1930s, single-beam sounders were used to make bathymetry maps. Today, multibeam echosounder
s (MBES) are typically used, which use hundreds of very narrow adjacent beams (typically 256) arranged in a fan-like swath
of typically 90 to 170 degrees across. The tightly packed array of narrow individual beams provides very high angular resolution
and accuracy. In general, a wide swath, which is depth dependent, allows a boat to map more seafloor in less time than a single-beam echosounder by making fewer passes. The beams update many times per second (typically 0.1–50 Hz
depending on water depth), allowing faster boat speed while maintaining 100% coverage of the seafloor. Attitude sensors allow for the correction of the boat's roll and pitch
on the ocean surface, and a gyrocompass provides accurate heading information to correct for vessel yaw
. (Most modern MBES systems use an integrated motion-sensor and position system that measures yaw as well as the other dynamics and position.) A boat-mounted Global Positioning System
(GPS) (or other Global Navigation Satellite System (GNSS)) positions the soundings with respect to the surface of the earth. Sound speed profiles (speed of sound in water as a function of depth) of the water column correct for refraction or "ray-bending" of the sound waves owing to non-uniform water column characteristics such as temperature, conductivity, and pressure. A computer system processes all the data, correcting for all of the above factors as well as for the angle of each individual beam. The resulting sounding measurements are then processed either manually, semi-automatically or automatically (in limited circumstances) to produce a map of the area. a number of different outputs are generated, including a sub-set of the original measurements that satisfy some conditions (e.g., most representative likely soundings, shallowest in a region, etc.) or integrated Digital Terrain Models
(DTM) (e.g., a regular or irregular grid of points connected into a surface). Historically, selection of measurements was more common in hydrographic
applications while DTM construction was used for engineering surveys, geology, flow modeling, etc. Since ca. 2003–2005, DTMs have become more accepted in hydrographic practice.
Satellites are also used to measure bathymetry. Satellite radar maps deep-sea topography by detecting the subtle variations in sea level caused by the gravitational pull of undersea mountains, ridges, and other masses. On average, sea level is higher over mountains and ridges than over abyssal plains and trenches.
In the United States
the United States Army Corps of Engineers
performs or commissions most surveys of navigable inland waterways, while the National Oceanic and Atmospheric Administration
(NOAA) performs the same role for ocean waterways. Coastal bathymetry data is available from NOAA's National Geophysical Data Center
(NGDC), which is now merged into National Centers for Environmental Information
. Bathymetric data is usually referenced to tidal vertical datum
s.NCEI -Coastal relief models
/ref> For deep-water bathymetry, this is typically Mean Sea Level (MSL), but most data used for nautical charting is referenced to Mean Lower Low Water (MLLW) in American surveys, and Lowest Astronomical Tide (LAT) in other countries. Many other datums are used in practice, depending on the locality and tidal regime.
Occupations or careers related to bathymetry include the study of oceans and rocks and minerals on the ocean floor, and the study of underwater earthquakes or volcanoes. The taking and analysis of bathymetric measurements is one of the core areas of modern hydrography, and a fundamental component in ensuring the safe transport of goods worldwide.
Overview for underwater terrain, data formats, etc.
High resolution bathymetry for the Great Barrier Reef and Coral Sea
Bathymetric Data Viewer from NOAA's NCEI
* ttp://www.floodmap.net/?ll=7.026133,10.861098&z=2&e=-1000 Interactive Web Map, Set Negative Elevation for Bathymetry