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Deposition of stream load occurs when the velocity of the stream decreases, causing the stream to lose the energy needed to carry sediment. As a result, sediment particles are deposited on the streambed or banks. This typically happens in areas where the stream's slope decreases or the stream widens.
The polar jet stream is generally stronger and faster-moving than the subtropical jet stream. The polar jet stream forms at higher latitudes and is located closer to the poles, while the subtropical jet stream is located at lower latitudes. The polar jet stream is associated with larger temperature contrasts and stronger pressure gradients, resulting in stronger winds compared to the subtropical jet stream.
The source of a stream is called a headwater or headstream. This is where the stream initially begins, often from a spring or melting snow.
Stream deposition occurs when a flowing stream loses energy, causing it to slow down and deposit sediment that it was previously carrying. This commonly occurs when the stream enters a flatter area, like a floodplain or a lake. As the stream's velocity decreases, it can no longer transport sediment, leading to deposition.
A stream carries materials through a process called erosion, where water and sediments are transported downstream. The flow of water in a stream can dislodge and carry rocks, soil, and other debris, along with any pollutants present, to be deposited in another location. The speed and volume of water in a stream can impact how much material it can carry.
Glen P. Bergstrom has written: 'Stream flow characteristics and calibration of the Tri-Creeks subwatersheds (1968-1977)' -- subject(s): Stream measurements
Clyde J Sholar has written: 'Calibration and verification of a streamflow simulation model for the Kentucky River near Lexington and Frankfort, Kentucky' -- subject(s): Stream measurements
A mature stream.
There are two common types. One uses UV-B (or other less characteristic radiation) absorption, and infers ozone concentration from the Beer-Lambert law. Good for measuring ozone in a gas stream. Another uses a compound that is oxidized by ozone, and this reaction causes / enables an electrical current flow. Good for measuring ozone gas in air or a liquid stream. These sensors usually require replacement / refreshment of the liquid in the cell, more frequent calibration, and are usually not ion specific to ozone (chlorine will also be indicated) so variable water quality can make calibration a problem.
A stream bed is the bottom (floor) of the stream.
Art stream
The stream reach is the length of the stream you have selected for monitoring.
The Limpid Stream was created in 1935.
It is occasionally called a sinking stream or a disappearing stream, but geographers and geologists normally call it a stream, just like another stream.
Lowering a stream's base level will cause the stream to do what?
an old stream is a deep wide and curvy river stream
The mouth of a stream is where the stream flows out into a larger body of water.