The storage and release of water from a large glacier-dammed lake
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The storage and release of water from a large glacier-dammed lake Russell Lake near Yakutat, Alaska, 1986

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Published by U.S. Dept. of the Interior, Geological Survey, Books and Open-File Reports Section, distributor in Denver, Colo .
Written in English

Subjects:

  • Glacial lakes -- Alaska -- Yakutat Region,
  • Dam failures -- Alaska -- Yakutat Region,
  • Water levels -- Russell Fiord (Alaska).

Book details:

Edition Notes

Includes bibliographical references (p. 7)

Statementby Harold R. Seitz, Donald S. Thomas, and Bud Tomlinson ; prepared in cooperation with the U.S. Department of Agriculture, Forest Service
SeriesOpen-file report -- 86-545, U.S. Geological Survey open-file report -- 86-545
ContributionsThomas, Donald S, Tomlinson, Bud, United States. Forest Service, Geological Survey (U.S.)
The Physical Object
FormatMicroform
Pagination1 microfiche
ID Numbers
Open LibraryOL13612834M

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During the outburst flood of a glacier-dammed lake on Gornergletscher, Switzerland, in July , the drained lake water triggered anomalous glacier motion. Glacial-lake floods occur when the dams forming the glacial lakes fail and release the water producing a surge of water downstream (ICIMOD, ). For this reason, they have similar effects as the dam-break floods discussed in Section The dams may form either due to the blockage of ice at the outflow of the glacier, similar to ice jams. A jökulhlaup is an Icelandic word for a glacier outburst flood that has been adopted by the English language and is now used to describe any large and abrupt release of water from a subglacial or proglacial lake/reservoir. It was triggered by the sudden release of about X m3 of water from moraine-dammed Klattasine Lake. The escaping waters breached the moraine, mobilized large quantities of sediment in the valley below the lake, and generated a debris flow, with an estimated volume of 2 4 X m3, that travelled in one or more surges 8 km to the mouth of Cited by:

  The event is known as jökulhlaup, an Icelandic term describing a sudden water release from glaciers or glacier-dammed lakes. Snow River flooding .   Seitz HR, Thomas DS, Tomlinson B () The storage and release of water from a large glacier-dammed lake: Russell Lake near Yakutat, Alaska, U.S. Geological Survey Open-File Report 86–, p 10 Google ScholarAuthor: Gheorghe Romanescu, Cristian Constantin Stoleriu, Andrei Enea. Full text of "Kenai Fjords National Park: Natural resource condition assessment" See other formats.   In the lake had begun to form, second image, but was less than 30 m across. The upper glacier was a smooth expanse of snow. By the lake was evident, and was 75 meters long. In the lake had expanded to a length of meters. By the lake was m in length, and had some thin icebergs broken off from the glacier front.

Managing Lakes and Reservoirs Caldera lake: a large, usually deep basin that forms in the center of an inactive volcano. ^ Volcanic* Volcanic activity creates lakes when water fills an inactive caldera (large crater) (Crater Lake, Oregon) or when lava flows dam up . Ice-water interactions during floods from Grænalón glacier-dammed lake, Iceland. Annals of Glaciol InternationalAssociation of Hydrological Sciences Red Book Publication Monitoring glacier mass balance can provide a seasonal measure of water accumulation, storage, and loss, which is useful for extrapolation to the greater population of glaciers in the region (Riedel and Burrows, ). Level One: Equilibrium Line Altitude and Accumulation-Area Ratio. The water cycle of a basin is affected by regional climate, topography, and human activities [1,2,3,4].Global warming has accelerated the regional water cycle and has changed the rainfall–runoff process in mountainous areas, resulting in changes in runoff recharge from glacier meltwater and precipitation [].For extremely arid areas with sparse precipitation, meltwater is the main recharging Author: Xiaofei Ma, Wei Yan, Chengyi Zhao, Zbigniew W. Kundzewicz.