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EspañolGLACIAL LAKE OUTBURST FLOOD
(Redirected from Jökulhlaup)
A 'glacial lake outburst flood' (GLOF), also known as a ''jökulhlaup'' in Icelandic (A ''jökulhlaup'' is technically a sudden and often catastrophic flood that occurs during a volcanic eruption, but is also used to describe other sorts of glacial flooding), can occur when a lake contained by a glacier or a terminal moraine dam fails. This can happen due to erosion, a buildup of water pressure, an avalanche of rock or heavy snow, an earthquake or cryoseism, or if a large enough portion of a glacier breaks off and massively displaces the waters in a glacial lake at its base.
A Jökulhlaup is a glacier outburst flood, principally from an ice-dammed lake. Jokulhlaup is an Icelandic term that has been adapted into the English language, and originally only referred to a glacier outburst flood triggered by a volcanic eruption, but now is accepted to describe any abrupt release of water dammed by a glacier.
Jökulhlaups have also been known to occur when a volcano erupts under a glacier. The ice over the volcano melts because of the heat, causing water to form a lake under the remaining ice-cap. Then the ice-cap collapses or the water breaks through the barrier in front of it, and there follows a more or less disastrous flooding of the land below the mountain. These events are similar to a type of lahar.
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 kilometers (68 miles) northeast of Kathmandu, Nepal, at an altitude of 4580 m (15,026 ft). The lake is dammed by a 150 m (492 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]
The most famous are the immense Jokulhlaup released from the Vatnajokul Ice Cap in Iceland. It is not by chance that the term Jökulhlaup comes from the Icelandic, as the south of Iceland has very often been victim to such catastrophes. This was the case when in 1996, 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 45,000 cubic meters per second, and destroyed parts of the Hringvegur (road no. 1). After the flooding some icebergs 10 m 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 Grimsvotn Volcanic Crater in the center of the Vatnajokul 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 outburst was very large yielding 6,000 cubic meters per second at peak flow.
Some jokulhlaups 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, 1972).
Almost every year, GLOFs occur in two locations in southeast section of Alaska. 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.[3]
Immense prehistoric GLOFs, known as the Missoula Floods, occurred in North American's Columbia River watershed towards 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.
A GLOF occurred September 6 to September 12 2003, from Grasshopper Glacier in the Wind River Mountains, Wyoming. Flow at the gauge site, 14 miles (23 km) downstream, rose from 7.1 m³/s (250 feet³/s) base flow to a peak of 37 m³/s (1,300 feet³/s) on September 9. The Downs' Fork Bridge was over-topped, woody debris was left on the bridge, and its abutments were damaged.[4]
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 [5]
In 1994 a jokulhlaup occurred at Farrow Creek, British Columbia[6]
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.[7].
It has been suggested [8] that Heinrich events during last glaciation could have been caused by gigantic jökulhlaups from a Hudson Bay lake dammed by ice at the mouth of Hudson Strait.
GLOFs occur with regularity in the valleys and low lying river plains of Bhutan.[9]
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.[10] In October 1994, a GLOF 90 kilometers upstream from Punakha Dzong caused massive flooding on the Pho Chhu River, damaging the dzong and causing casualties.10
The English Channel 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.[11]
★ Post, A. and L.R. Mayo (1972) Glacier Dammed Lakes and Outburst Floods in Alaska. Anchorage, Alaska U.S. Geological Survey, Denver CO.
1. http://www.un.org/Pubs/chronicle/2002/issue3/0302p48_glacial_lakes_flood_threat.html
2. http://www.dhm.gov.np/tsorol/background.htm
3. Aimee Devaris. Southeast Alaska Jökulhlaups. Retrieved on 2006-12-03.
4. http://www.watershed.org/wmc/modules.php?op=modload&name=News&file=article&sid=13
5. Kicking Horse Pass – 1978 Environment Canada
6. The 1994 jokulhlaup at Farrow Creek, British Columbia, Canada, , , , Geomorphology, 1997
7. Limnology, sedimentology, and hydrology of a jökulhlaup into a meromictic high arctic lake, , , , Canadian Journal of Earth Sciences, accepted
8.
Hudson Bay-Hudson Strait jökulhlaups and Heinrich events: a hypothesis, , , , Palaeogeography, Palaeoclimatology, Palaeoecology, 1995
9.
10.
11. "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)
★ Glacial Lake Outburst Flood Monitoring and Early Warning System
★ Mount Rainier Glacier Hazards and Glacial Outburst Floods
★ Southeast Alaska Jökulhlaups
★ Jokulhlaup at Grasshopper Glacier, Wind River Mountains, Wyoming
★ Small-scale glacial lake outburst flood, Lemon Glacier, Alaska
★ Enlarged Views of 2002 Russell Fiord Closure and Russell Lake Outburst
Hubbard Glacier, Alaska squeezes towards Gibert Point on May 20 2002. The glacier is close to sealing off Russell Fjord at top from Disenchantment Bay at bottom.
A 'glacial lake outburst flood' (GLOF), also known as a ''jökulhlaup'' in Icelandic (A ''jökulhlaup'' is technically a sudden and often catastrophic flood that occurs during a volcanic eruption, but is also used to describe other sorts of glacial flooding), can occur when a lake contained by a glacier or a terminal moraine dam fails. This can happen due to erosion, a buildup of water pressure, an avalanche of rock or heavy snow, an earthquake or cryoseism, 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 |
| Monitoring |
| Examples |
| Iceland |
| Alaska |
| Contiguous United States |
| Canada |
| Bhutan |
| England/France |
| References |
| Printed Media |
| World Wide Web |
| External links |
Definition
A Jökulhlaup is a glacier outburst flood, principally from an ice-dammed lake. Jokulhlaup is an Icelandic term that has been adapted into the English language, and originally only referred to a glacier outburst flood triggered by a volcanic eruption, but now is accepted to describe any abrupt release of water dammed by a glacier.
Jökulhlaups have also been known to occur when a volcano erupts under a glacier. The ice over the volcano melts because of the heat, causing water to form a lake under the remaining ice-cap. Then the ice-cap collapses or the water breaks through the barrier in front of it, and there follows a more or less disastrous flooding of the land below the mountain. These events are similar to a type of lahar.
Monitoring
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 kilometers (68 miles) northeast of Kathmandu, Nepal, at an altitude of 4580 m (15,026 ft). The lake is dammed by a 150 m (492 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 Jokulhlaup released from the Vatnajokul Ice Cap in Iceland. It is not by chance that the term Jökulhlaup comes from the Icelandic, as the south of Iceland has very often been victim to such catastrophes. This was the case when in 1996, 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 45,000 cubic meters per second, and destroyed parts of the Hringvegur (road no. 1). After the flooding some icebergs 10 m 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 Grimsvotn Volcanic Crater in the center of the Vatnajokul 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 outburst was very large yielding 6,000 cubic meters per second at peak flow.
Alaska
Some jokulhlaups 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, 1972).
Almost every year, GLOFs occur in two locations in southeast section of Alaska. 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.[3]
Contiguous United States
Immense prehistoric GLOFs, known as the Missoula Floods, occurred in North American's Columbia River watershed towards 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.
A GLOF occurred September 6 to September 12 2003, from Grasshopper Glacier in the Wind River Mountains, Wyoming. Flow at the gauge site, 14 miles (23 km) downstream, rose from 7.1 m³/s (250 feet³/s) base flow to a peak of 37 m³/s (1,300 feet³/s) on September 9. The Downs' Fork Bridge was over-topped, woody debris was left on the bridge, and its abutments were damaged.[4]
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 [5]
In 1994 a jokulhlaup occurred at Farrow Creek, British Columbia[6]
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.[7].
It has been suggested [8] that Heinrich events during 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.[9]
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.[10] In October 1994, a GLOF 90 kilometers upstream from Punakha Dzong caused massive flooding on the Pho Chhu River, damaging the dzong and causing casualties.10
England/France
The English Channel 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.[11]
References
Printed Media
★ Post, A. and L.R. Mayo (1972) Glacier Dammed Lakes and Outburst Floods in Alaska. Anchorage, Alaska U.S. Geological Survey, Denver CO.
World Wide Web
1. http://www.un.org/Pubs/chronicle/2002/issue3/0302p48_glacial_lakes_flood_threat.html
2. http://www.dhm.gov.np/tsorol/background.htm
3. Aimee Devaris. Southeast Alaska Jökulhlaups. Retrieved on 2006-12-03.
4. http://www.watershed.org/wmc/modules.php?op=modload&name=News&file=article&sid=13
5. Kicking Horse Pass – 1978 Environment Canada
6. The 1994 jokulhlaup at Farrow Creek, British Columbia, Canada, , , , Geomorphology, 1997
7. Limnology, sedimentology, and hydrology of a jökulhlaup into a meromictic high arctic lake, , , , Canadian Journal of Earth Sciences, accepted
8.
Hudson Bay-Hudson Strait jökulhlaups and Heinrich events: a hypothesis, , , , Palaeogeography, Palaeoclimatology, Palaeoecology, 1995
9.
10.
11. "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)
External links
★ Glacial Lake Outburst Flood Monitoring and Early Warning System
★ Mount Rainier Glacier Hazards and Glacial Outburst Floods
★ Southeast Alaska Jökulhlaups
★ Jokulhlaup at Grasshopper Glacier, Wind River Mountains, Wyoming
★ Small-scale glacial lake outburst flood, Lemon Glacier, Alaska
★ Enlarged Views of 2002 Russell Fiord Closure and Russell Lake Outburst
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