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The Agua Fria River (Spanish for "cold water") is a 120-mile (190 km) long intermittent stream which flows generally south from 20 miles (32 km) east-northeast of Prescott in the U.S. state of Arizona. Prescott draws much of its municipal water supply from the upper Agua Fria watershed. [6] The Agua Fria runs through the Agua Fria National ...
The Big Sandy River flows year-round (perennial flow) south of the Signal Ghost Town site and intermittently above this site. [5] [6] In the period of 2007–2016, the surface water flow of the Big Sandy at the USGS monitoring site at the Signal Ghost Town ranged from a minimum of 22 US gallons (83 L) per second to a maximum output of nearly 524,000 US gallons (1,980,000 L) per second during ...
This flow creates a fast-moving rip current. A rip current (or just rip) is a specific type of water current that can occur near beaches where waves break. A rip is a strong, localized, and narrow current of water that moves directly away from the shore by cutting through the lines of breaking waves, like a river flowing out to sea. The force ...
Current events; Random article; ... List of rivers in Arizona , sorted ... USGS Hydrologic Unit Map - State of Arizona (1974)
The water in this stream forms varying currents as it makes its way downhill. In hydrology, a current in a water body is the flow of water in any one particular direction. The current varies spatially as well as temporally, dependent upon the flow volume of water, stream gradient, and channel geometry.
An example of a geostrophic flow in the Northern Hemisphere. A northern-hemisphere gyre in geostrophic balance. Paler water is less dense than dark water, but more dense than air; the outwards pressure gradient is balanced by the 90 degrees-right-of-flow coriolis force. The structure will eventually dissipate due to friction and mixing of water ...
The risk of strong rip currents is high at all the state’s beaches through the same period ... North Carolina beaches began posting red flags on Friday and warning swimmers not to go in the water.
The flow of Big Leroux Spring was measured in 1949 at 29 gallons per minute, while the average flow between 2004 and 2013 was 13.5 gallons per minute. During the 20th century, the springs had been modified and sequestered to provide water for the city and for different private owners, with underground pipes particularly reducing the flow.