Flash flood

Source: Wikipedia, the free encyclopedia.
An underpass in Charlottesville, Virginia, United States. during normal conditions (upper) and after fifteen minutes of heavy rain (lower)
Driving through a flash-flooded road
A flash flood after a thunderstorm in the Gobi, Mongolia

A flash flood is a rapid

debris dam, or a human structure such as a man-made dam, as occurred before the Johnstown Flood of 1889. Flash floods are distinguished from regular floods by having a timescale of fewer than six hours between rainfall and the onset of flooding.[1]

Flash floods are a significant hazard, causing more fatalities in the U.S. in an average year than lightning,

floodplains
and can be destructive of vegetation cover not adapted to frequent flood conditions.

Causes

Flash flooded road in Northern Mexico, after a 3–5 hour long thunderstorm that occurred during a drought that lasted nearly 1 year

Flash floods most often occur in dry areas that have recently received

tropical storms, as well as the sudden thawing effect of ice dams.[2][3] Human activities can also cause flash floods to occur. When dams fail, a large quantity of water can be released and destroy everything in its path.[3]

Hazards

A flash flood greatly inundates a small ditch, flooding barns and ripping out newly installed drain pipes.

The United States

hurricanes (16).[6]

In deserts, flash floods can be particularly deadly for several reasons. First, storms in arid regions are infrequent, but they can deliver an enormous amount of water in a very short time. Second, these rains often fall on poorly absorbent and often clay-like soil, which greatly increases the amount of runoff that rivers and other water channels have to handle.[7] These regions tend not to have the infrastructure that wetter regions have to divert water from structures and roads, such as storm drains, culverts, and retention basins, either because of sparse population or poverty, or because residents believe the risk of flash floods is not high enough to justify the expense. In fact, in some areas, desert roads frequently cross a dry river and creek beds without bridges. From the driver's perspective, there may be clear weather, when a river unexpectedly forms ahead of or around the vehicle in a matter of seconds.[8] Finally, the lack of regular rain to clear water channels may cause flash floods in deserts to be headed by large amounts of debris, such as rocks, branches, and logs.[9]

Deep slot canyons can be especially dangerous to hikers as they may be flooded by a storm that occurs on a mesa miles away. The flood sweeps through the canyon; the canyon makes it difficult to climb up and out of the way to avoid the flood. For example, a cloudburst in southern Utah on 14 September 2015 resulted in 20 flash flood fatalities, of which seven fatalities occurred at Zion National Park when hikers were trapped by floodwaters in a slot canyon.[10]

Flash flood impacts

Flash floods induce severe impacts in both the built and the natural environment. The effects of flash floods can be catastrophic and show extensive diversity, ranging from damages in buildings and infrastructure to impacts on vegetation, human lives and livestock. The effects are particularly difficult to characterize in urban areas.[11]

Researchers have used datasets such as the Severe Hazards Analysis and Verification Experiment (SHAVE) and the U.S. National Weather Service (NWS) Storm Data datasets to connect the impact of flash floods with the physical processes involved in flash flooding. This should increase the reliability of flash flood impact forecasting models.[12] Analysis of flash floods in the United States between 2006 and 2012 shows that injuries and fatalities are most likely in small, rural catchments, that the shortest events are also the most dangerous, that the hazards are greatest after nightfall, and that a very high fraction of injuries and fatalities involve vehicles.[13]......

An impact severity scale is proposed in 2020 providing a coherent overview of the flash flood effects through the classification of impact types and severity and mapping their spatial extent in a continuous way across the floodplain. Depending on the affected elements, the flood effects are grouped into 4 categories: (i) impacts on built environment (ii) impacts on man-made mobile objects,(iii) impacts on the natural environment (including vegetation, agriculture, geomorphology, and pollution) and (iv) impacts on the human population (entrapments, injuries, fatalities). The scale was proposed as a tool on prevention planning, as the resulting maps offer insights on future impacts, highlighting the high severity areas.[11]

Flash floods can cause rapid soil erosion.

Nile River.[15] However, flash floods of short duration produce relatively little bedrock erosion or channel widening, having their greatest impact from sedimentation on the floodplain.[16]

Some wetlands plants, such as certain varieties of rice, are adapted to endure flash flooding.[17] However, plants that thrive in drier areas can be harmed by flooding, as the plants can become stressed by the large amount of water.[18][19]

See also

References

  1. ^ "Flash Flooding Definition". National Weather Service. Archived from the original on September 1, 2017. Retrieved August 31, 2017.
  2. ^ WeatherEye (2007). "Flash Flood!". Sinclair Acquisition IV, Inc. Archived from the original on 2009-02-27. Retrieved 2009-09-09.
  3. ^ a b National Weather Service Forecast Office Morristown, Tennessee (2006-03-07). "Definitions of flood and flash flood". National Weather Service Southern Region Headquarters. Archived from the original on 2006-09-29. Retrieved 2009-09-09.
  4. National Weather Service. Archived from the original
    on 2008-01-11. Retrieved 2007-06-25.
  5. from the original on 2007-07-05. Retrieved 2007-06-25.
  6. ^ "Turn Around Don't Drown". Archived from the original on 2018-11-29. Retrieved 2007-06-25.
  7. .
  8. (PDF) on 2008-06-25. Retrieved 2008-07-17.
  9. ^ Jahns, R.H. (1949). "Desert floods" (PDF). Engineering and Science. 12 (8): 10–14. Archived (PDF) from the original on 30 April 2021. Retrieved 17 July 2021.
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Further reading

External links