In plants, the transpiration stream is the uninterrupted stream of water, and other, which is taken up by the roots and, via the xylem vessels, transported to the leaves where it will eventually evaporate into the air/applets-interface of the substomatal cavity. It is driven in by capillary action and in some plants root pressure. The main driving factor is the difference in water potential between the soil and the substomatal cavity caused by transpiration.
The jet stream
Stream gradient, or the slope of the stream channel, affects stream velocity by influencing the speed at which water flows downstream. A steeper stream gradient typically results in a faster water flow velocity, as the force of gravity pulls water downhill more strongly. Conversely, a gentler stream gradient leads to slower water flow velocity.
The mouth of a stream is where it meets a larger body of water, such as a lake, ocean, or another stream. It is where the stream's water flows out and mixes with the water of the larger body.
A continental jet-stream travels parallel to the equator - a polar jet-stream travels in a north/south direction.
dew, ice, stream and snow are all forms of water. Cold is not.
the finest canoes in the world
A mature stream.
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.
what is a spark stream
stream