Depth measurements in the sea are done with echo sounders, using an acoustic signal which is reflected off the bottom. Sound travels at about 1.5 km/sec in water. Echo sounders can be quite simple devices for use by yachts in shallow waters, to much more complex equipment used in surveys for geographic purposes. The process is known as Bathymetry and there is a Wikipedia article under this title for more information.
A sonar device is commonly used to emit sound waves and measure the ocean floor. Sonar works by sending sound waves downward, which bounce off the sea floor and return, providing information about the depth and characteristics of the ocean floor.
Since liquid pressure is function of density,acceleration due to gravity and depth of liquid level so here density of sea water is greater than that of river water ,so liquid pressure in sea must be more.
Pressure at a given depth of water can be calculated using a formula like, "#1 #1kgf/cm2." Therefore, water pressure at 2000 meters below sea level will be around 1.2 bar.
Simply by measuring the time it takes for the sonar 'ping' to return to the device that sent it. The speed of sound is constant - and dividing the time by the speed of sound gives the distance !
A depth of approximately 10 meters is required in sea water for 1 bar pressure. This is because each meter of water depth exerts a pressure of approximately 0.1 bar due to the weight of the water above it.
Tjehs
fathometer is an instrument used to measure the altitude of na object above a fixed level , fathometer measures the sea depth
The instrument used to measure the depth of the sea is called a bathymeter or echo sounder. It sends sound waves to the ocean floor and measures the time it takes for the sound waves to bounce back, allowing for the calculation of water depth.
Sea level
A fathom is a unit of imperial length which is used to measure the depth of water. I fathom is equivalent to 6feet or 1.83metres e.g. 3 fathoms = 18ft or 5.49m
Scientists measure ocean depths using sonar technology, which involves sending sound waves into the water and measuring how long it takes for them to bounce back. Another method is using satellite altimetry, which measures the sea surface height and then estimates the depth based on the gravitational pull of underwater features. Submersibles equipped with depth sensors can also be used to directly measure the depth of the seafloor.
an ultrasound wave is beamed down from a boat and then the wave bounces back from the seabed to a reciever. the longer the wave takes, the deeper the water.
no human can live in the depth sea
the density of sea increases with depth
bathometer
Traditionally the unit is the fathom (=6 feet) but nowadays you will see metres or indeed any proper unit of length.
no human being can live on the depth sea