hunter, Nick, and Spencer
During dry spells, stream flow is typically reduced due to decreased rainfall and lower groundwater levels. This can lead to streams drying up in some cases, impacting aquatic ecosystems and water availability for surrounding areas. It is important to monitor stream flow during dry spells to assess water resources and potential ecological impacts.
Some choices: flow, stream, deluge, flood, gush
It's the flow of water that carries solids, whenever the flow slows then some of the solids will fall to the bottom of the stream.
In some rare cases a river could flow into the ground and dry up completely at the Small rivers may be called by several other names, including stream, creek.
With other streams or tributaries joining, a stream's flow of water increases until it can be considered a river. For example, the mighty Mississippi starts out as a trickle of water near the Canadian border. Many similar trickles begin to join it and the flow increases.
some different types of monitor are flat panel monitor and CRT monitor (saad ashfaq)
The following are some important reasons why large companies' documents has to be managed; to monitor the effectiveness or efficiency of their services, to determine the profit and cost or expenses-avoidance, and to state their social and moral responsibilities.
No, "poor" and "pour" are not homophones. "Poor" refers to lacking wealth or resources, while "pour" means to flow or cause to flow in a steady stream.
A stream is a flowing body of Waterwith a Current_(stream), confined within a Stream_bedand Stream_bank. Depending on its locale or certain characteristics, a stream may be referred to as a branch, brook, beck, Burn_(topography), creek, Kill_(body_of_water),Lick_(stream),Rill,Riversyke, Bayou, rivulet, or run. In some countries or communities a stream may be defined by its size. In the United_Statesa stream is classified as a watercourse less than 60 feet (18 metres) wide.
A stream is a flowing body of liquid, typically water, which is in its liquid state.
Not necessarily. The lag time between the center of mass of a storm and peak stream discharge can vary depending on factors such as storm intensity, duration, topography, and soil conditions. In some cases, the peak discharge of a stream can occur before, during, or after the storm event.