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This study addresses the delineation of areas that contribute baseflow to a stream reach, also known as stream capture zones.
Generally, ecosystems have been described at the level of the landscape patch or stream reach composed of a relatively distinct community type.
Calculating discharge from a stream reach by HSPF is based mainly on function tables (FTABLEs), which describe the relationship between surface area, stream stage, volume, and discharge.
We found that ecoregions afforded a good spatial structure that can help in understanding longitudinal trends in stream reach morphology surveyed at the reach scale.
Temperature variation is primarily driven by solar radiation, while landscape topography, geology, and stream reach processes across ecosystem scales contribute to local variability.
Bank erosion ranges from 0 to 470 kg/m/y and floodplain sedimentation ranges from 18 to 1369 kg/m/y (m refers to meters of stream reach).
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The jet stream reaches its greatest velocity at the tropopause.
On several occasions a lava stream reached the shores of Lake Kivu.
The HTTP response is not closed by the server until the stream reaches its end.
The stream reaches the optimal conditions in the CPU for transportation.
This autogenic process decreases sinuosity and increases channel slope, stream power, and the potential to incise along adjacent stream reaches.
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