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definition - Glacial_Lake_Outburst_Flood

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Glacial lake outburst flood

                   
  Hubbard Glacier, Alaska squeezes towards Gibert Point on 20 May 2002. The glacier is close to sealing off Russell Fjord (top) from Disenchantment Bay (below).

A glacial lake outburst flood (GLOF) is a type of outburst flood that occurs when the dam containing a glacial lake fails. The dam can consist of glacier ice or a terminal moraine. Failure can happen due to erosion, a buildup of water pressure, an avalanche of rock or heavy snow, an earthquake or cryoseism, volcanic eruptions under the ice, or if a large enough portion of a glacier breaks off and massively displaces the waters in a glacial lake at its base.

Contents

  Definition

  In this Hubbard Glacier image from 16 July 2002, the glacier has closed off Russell Fjord from Disenchantment Bay. The waters behind the glacier rose 61 feet (19 m) in 10 weeks, creating a short lived Russell Lake.

A glacial lake outburst flood is a type of outburst flood occurring when water dammed by a glacier or a moraine is released. A water body that is dammed by the front of a glacier is called a marginal lake, and a water body that is capped by the glacier is called a sub-glacial lake. When a marginal lake bursts, it may also be called a marginal lake drainage. When a sub-glacial lake bursts, it may be called a jökulhlaup.

A jökulhlaup is thus a sub-glacial outburst flood. Jökulhlaup is an Icelandic term that has been adopted into the English language, originally referring only to glacial outburst floods from Vatnajökull, which are triggered by volcanic eruptions, but now is accepted to describe any abrupt and large release of sub-glacial water.

Glacial lake volumes vary, but may hold millions to hundreds of millions of cubic metres of water. Catastrophic failure of the containing ice or glacial sediment can release this water over periods of minutes to days. Peak flows as high as 15,000 cubic metres per second have been recorded in such events, suggesting that the v-shaped canyon of a normally small mountain stream could suddenly develop an extremely turbulent and fast-moving torrent some 50 metres (160 ft) deep. On a downstream floodplain, it suggests a somewhat slower inundation spreading as much as 10 kilometres (6.2 mi) wide. Both scenarios are significant threats to life, property and infrastructure.

  Monitoring

  The Hubbard Glacier is overwhelmed on 14 August 2002 in the second largest GLOF in historical times.

The United Nations has a series of monitoring efforts to help prevent death and destruction in regions that are likely to experience these events. The importance of this situation has magnified over the past century due to increased populations, and the increasing number of glacial lakes that have developed due to glacier retreat. While all countries with glaciers are susceptible to this problem, central Asia, the Andes regions of South America and those countries in Europe that have glaciers in the Alps, have been identified as the regions at greatest risk.[1]

There are a number of imminent deadly GLOFs situations that have been identified worldwide. The Tsho Rolpa glacier lake is located in the Rolwaling Valley, about 110 kilometres (68 mi) northeast of Kathmandu, Nepal, at an altitude of 4,580 metres (15,030 ft). The lake is dammed by a 150 metres (490 ft) high unconsolidated terminal moraine dam. The lake is growing larger every year due to the melting and retreat of the Trakarding Glacier, and has become the largest and most dangerous glacier lake in Nepal, with approximately 90 to 100 million m³ (117 to 130 million yd³) of water stored.[2]

  Examples

  Iceland

  Remains of a steel bridge in Skaftafell National Park after a glacial outburst

The most famous are the immense jökulhlaup released from the Vatnajökull Ice Cap in Iceland. It is not by chance that the term jökulhlaup (jökull = glacier, hlaup = run (n.)/running[3]) comes from Icelandic, as the south of Iceland has very often been the victim of such catastrophes. This was the case in 1996, when the volcano under the Grímsvötn lakes belonging to the Vatnajökull glacier erupted, and the river Skeiðará flooded the land in front of Skaftafell National Park. The jökulhlaup reached a flow rate of 50,000 cubic metres per second, and destroyed parts of the Hringvegur (Ring Road or Iceland Road #1). The flood carried ice floes that weighed up to 5000 tons with icebergs between 100–200 tons striking the Gigjukvisl Bridge of the Ring Road (the ruins are well marked with explanatory signs today as a popular tourist stop). The tsunami released was up to 4 metres (13 ft) high and 600 metres (660 yd) wide. The flood carried with it 185 million tons of silt.[4] The jökulhlaup flow made it for several days the 2nd largest river (in terms of water flow) after the Amazon.

After the flooding, some icebergs 10 metres (33 ft) high could be seen on the banks of the river where the glacier run had left them behind (see also Mýrdalsjökull). The peak water release from a lake that develops around the Grímsvötn Volcanic Crater in the center of the Vatnajökull ice cap generates flows that exceed the volume of the Mississippi River. The outbursts have occurred in 1954, 1960, 1965, 1972, 1976, 1982, 1983, 1986, 1991 and 1996. In 1996, the eruption melted 3 cubic kilometres (0.72 cu mi) of ice and yielded an outburst of 6,000 cubic metres (7,800 cu yd) per second at peak flow.

  Alaska

Some jökulhlaups release annually. Lake George near the Knik River had large annual outbreaks from 1918 to 1966. Since 1966 the Knik Glacier has retreated and an ice-dam is no longer created. Lake George might resume annual floods if the glacier thickens again and blocks the valley (Post and Mayo, 1971). Almost every year, GLOFs occur in two locations in southeastern Alaska, one of which is Abyss Lake. The releases associated with the Tulsequah Glacier near Juneau often inundate a nearby airstrip. About 40 cabins could potentially be affected and a few have been damaged by the larger floods. Events from Salmon Glacier near Hyder have damaged roads near the Salmon River.[5]

  Contiguous United States

Immense prehistoric GLOFs, known as the Missoula Floods, occurred in North America's Columbia River watershed toward the end of the last ice age. They were the result of periodic breaches of ice dams in present day Montana, resulting in the draining of a body of water now known as Glacial Lake Missoula. The immense floods scoured the Columbia Plateau as the water raced toward the ocean, resulting in the Channeled Scablands topography that exists today across Central and Eastern Washington.

Glacial River Warren drained Glacial Lake Agassiz during the Wisconsinian glaciation; the now mild Minnesota River flows through its bed. This river seasonably drained glacial meltwater into what is now the Upper Mississippi River. The region now termed the Driftless Area of North America was contemporaneously also subject to glacial outburst floods from Glacial Lake Grantsburg, and Glacial Lake Duluth during all three phase of the last ice age.

Between 6 and 10 September 2003, a GLOF occurred from Grasshopper Glacier in the Wind River Mountains, Wyoming. A proglacial lake at the head of the glacier burst through a glacial dam, and water from the lake carved a trench down the center of the glacier for more than 0.8 kilometres (0.5 mi). An estimated 2,460,000 cubic metres (650,000,000 US gal) gallons of water were released in four days, raising the flow level of Dinwoody Creek from 5.66 cubic metres (200 cu ft) per second to 25.4 cubic metres (900 cu ft) per second, as recorded at a gauging station 27 kilometres (17 mi) downstream. Debris from the flood was deposited more than 32 kilometres (20 mi) along the creek. The GLOF has been attributed to the rapid retreat of the glacier, which has been ongoing since the glacier was first accurately measured in the 1960s.[6][7]

  Canada

In 1978 debris flows triggered by a jökulhlaup from Cathedral Glacier destroyed part of the Canadian Pacific railway track, derailed a freight train and buried parts of the Trans Canada Highway[8]

In 1994 a jökulhlaup occurred at Farrow Creek, British Columbia.[9]

In 2003 a jökulhlaup drained into Lake Tuborg on Ellesmere Island, and the events and its aftermath were monitored. The ice-dammed lake drained catastrophically by floating its ice dam. This is an extremely rare occurrence in the Canadian High Arctic, where most glaciers are cold based, and ice-dammed lakes typically drain slowly by overtopping their dams.[10]

It has been suggested[11] that the Heinrich events during the last glaciation could have been caused by gigantic jökulhlaups from a Hudson Bay lake dammed by ice at the mouth of Hudson Strait.

  Bhutan

GLOFs occur with regularity in the valleys and low lying river plains of Bhutan.[12] In the recent past, flash floods have occurred in the Thimphu, Paro and Punankha-Wangdue valleys. Of the 2674 glacial lakes in Bhutan, 24 have been identified by a recent study as candidates for GLOFs in the near future.[13] In October 1994, a GLOF 90 kilometres (56 mi) upstream from Punakha Dzong caused massive flooding on the Pho Chhu River, damaging the dzong and causing casualties.[13]

  England/France

The Strait of Dover is thought to have been created around 200,000 years ago by a catastrophic GLOF caused by the breaching of the Weald-Artois Anticline, which acted as a natural dam that held back a large lake in the Doggerland region, now submerged under the North Sea. The flood would have lasted several months, releasing as much as one million cubic metres of water per second. The cause of the breach is not known but may have been caused by an earthquake or simply the build-up of water pressure in the lake. As well as destroying the isthmus that connected Britain to continental Europe, the flood carved a large bedrock-floored valley down the length of the English Channel, leaving behind streamlined islands and longitudinal erosional grooves characteristic of catastrophic megaflood events.[14]

  Nepal

Even though GLOF events have been occurring in Nepal for many decades, the Dig Cho glacial lake outburst, which took place in 1985, has triggered detailed study of this phenomenon. In 1996, the Water and Energy Commission Secretariat (WECS) of Nepal reported that five lakes were potentially dangerous, namely, Dig Tsho, Imja, Lower Barun, Tsho Rolpa, and Thulagi, all lying above 4100 m. A recent study done by ICIMOD and UNEP (UNEP, 2001) reported 20 potentially dangerous lakes in Nepal. In ten of them GLOF events have occurred in the past few years and some have been regenerating after the event. Additional dangerous glacial lakes may exist in parts of Tibet that are drained by streams crossing into Nepal, raising the possibility of outburst incidents in Tibet causing downstream damage in Nepal. The Gandaki River basin is reported to contain 1025 glaciers and 338 lakes.

Thulagi glacier The Thulagi glacier, which is located in the Upper Marsyangdi River basin, is one out of the two moraine-dammed lakes (supra-glacial lakes), identified as a potentially dangerous lake. The KfW, Frankfurt, the BGR (Federal Institute for Geosciences and Natural Resources, Germany), in cooperation with the Department of Hydrology and Meteorology in Kathmandu, have carried out studies on the Thulagi Glacier and have concluded that even assuming the worst case, a disastrous outburst of the lake can be excluded in the near future.[15]

  Pakistan

In 1929 a GLOF from the Chong Khumdan Glacier in the Karakoram caused flooding on the Indus River 1,200 km downstream (a maximum flood rise of 8.1 m at Attock).[16]

  China

Longbasaba and Pida lakes are two moraine-dammed lakes at an altitude of about 5700 m in the Chinese Himalayas. Due to the rise of temperature, the areas of the Longbasaba and Kaer glaciers decreased by 8.7% and 16.6% from 1978 to 2005. Water from glaciers directly flowed into Longbasaba and Pida lakes, and the area of the two lakes increased by 140% and 194%. According to the report of the Hydrological Department of the Tibet Autonomous Region (HDTAR) in 2006, if a GLOF had occurred at the two lakes, 23 towns and villages, where more than 12,500 people live, would have been endangered.[17]

In Tibet, one of the major barley producing areas of the Tibetan Plateau was destroyed by GLOFs in August 2000. More than 10,000 homes, 98 bridges and dykes were destroyed and its estimated cost was about $75 million. The farming communities faced food shortages that year by losing their grain and livestock.[18]

A major GLOF was reported in 1978 in the valley of the Shaksgam River in the Chinese Karakoram.[16]

  See also

  References

  1. ^ UN Chronicle | Global Warming Triggers Glacial Lakes Flood Threat
  2. ^ http://www.dhm.gov.np/tsorol/background.htm
  3. ^ Icelandic online dictionary
  4. ^ [Stefán Benediktsson and Sigrún Helgadóttir, “The Skeiđarđá River in Full Flood 1996,” Skaftafell National Park: Environment and Food Agency, UST, March, 2007-->]
  5. ^ Aimee Devaris. Southeast Alaska Jökulhlaups. Retrieved on 2006-12-03.
  6. ^ Thuermer, Angus (2004). "The day the Grasshopper burped". Jackson Hole News and Guide. http://www.jhnews.com/Archives/Environmental/031105-enviro.html. Retrieved 2007-10-31. 
  7. ^ Oswald, Liz; Ellen Wohl (2007). "Jökulhlaup in the Wind River Mountains, Shoshone National Forest, Wyoming". Advancing the Fundamental Sciences: A Selection of Presentations for Forest Service Earth Scientists. U.S. Forest Service. http://stream.fs.fed.us/afsc/pdfs/Oswald.pdf. Retrieved 2009-12-17. 
  8. ^ Environment Canada. "Kicking Horse Pass – 1978". Flooding events in Canada - British Columbia. http://www.ec.gc.ca/water/en/manage/floodgen/e_bc.htm. 
  9. ^ Clague, J.J.; Evans, S.G. (1997). "The 1994 jökulhlaup at Farrow Creek, British Columbia, Canada". Geomorphology 19 (1): 77–87. Bibcode 1997Geomo..19...77C. doi:10.1016/S0169-555X(96)00052-9. 
  10. ^ Lewis, T.; Francus, P.; Bradley, R.S. (2007). "Limnology, sedimentology, and hydrology of a jökulhlaup into a meromictic high arctic lake". Canadian Journal of Earth Sciences 44 (6): 791–806. Bibcode 2007CaJES..44..791L. doi:10.1139/E06-125. http://www.geo.umass.edu/grads/lewist/#Publications. 
  11. ^ Johnson, R.G.; S.-E. Lauritzen (1995). "Hudson Bay-Hudson Strait jökulhlaups and Heinrich events: a hypothesis". Palaeogeography, Palaeoclimatology, Palaeoecology 117 (1): 123–137. doi:10.1016/0031-0182(94)00120-W. 
  12. ^ Chhopel, Karma (2006-03-15). "Flash Floods and Debris Flows due to Glacial Lake Outburst Floods" (ppt). Proceedings of the International Workshop on Flash Flood Forecasting coordinated by the U.S. National Oceanic and Atmospheric Administration's National Weather Service and the World Meteorological Organization, San José, Costa Rica, March 2006. Conference web site (NOAA), Abstract (pdf). Thimphu, Bhutan: Hydro-Met Services Division, Dept. of Energy, Ministry of Trade and Industry. http://www.nws.noaa.gov/iao/FFW/2006/Presentations/Session%207/CHHOPHEL-BHUTAN.ppt. 
  13. ^ a b Wangda, Dorji (2006-09-09). "GIS Tools Demonstration: Bhutan Glacial Hazards" (pdf). Proceedings of the LEG Regional Workshop on NAPA coordinated by UNITAR, Thimphu, Bhutan, September 2006. Conference web site (UNITAR). Dept, of Geology and Mines, Govt. of Bhutan. http://www.unitar.org/ccp/bhutan/06-%20BhutanGlacialhazards-GIS%20demo.pdf. 
  14. ^ "Catastrophic flooding origin of shelf valley systems in the English Channel". Sanjeev Gupta, Jenny S. Collier, Andy Palmer-Felgate & Graeme Potter. Nature 448, 342-345 (19 July 2007)
  15. ^ BGR/NLfB/GGA: Gletschersee Thulagi
  16. ^ a b Hewitt, K. (1982) Natural dams and outburst floods of the Karakoram Himalaya
  17. ^ Wang, Xin et al. “Assessment and Simulation of Glacier Lake Outburst Floods for Longbasaba and Pida Lakes, China” Mountain Research and Development 28.3: 310-17. 2008
  18. ^ WWF Nepal Program. “An Overview of Glaciers, Glacier Retreat, and Subsequent Impacts in Nepal, India and China”. 14 March. 2005
  • Post, A. and L.R. Mayo (1971) Glacier Dammed Lakes and Outburst Floods in Alaska. HYDROLOGIC INVESTIGATIONS ATLAS HA-455. Anchorage, Alaska U.S. Geological Survey, Denver CO. [1]
  • Rudoy A.N. (1998) Mountain Ice-Dammed Lakes of Southern Siberia and their Influence on the Development and Regime of the Runoff Systems of North Asia in the Late Pleistocene. Chapter 16. (P. 215—234.) — Palaeohydrology and Environmental Change / Eds: G. Benito, V.R. Baker, K.J. Gregory. — Chichester: John Wiley & Sons Ltd. 353 p.

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