Sand dunes and valley fills from Preboreal glacial‐lake outburst floods in south‐eastern Norway – beyond the aeolian paradigm

Sedimentology ◽  
2019 ◽  
Vol 67 (2) ◽  
pp. 810-848 ◽  
Author(s):  
Louise Hansen ◽  
Georgios Tassis ◽  
Fredrik Høgaas
Keyword(s):  
Sand Dunes ◽  
Glacial Lake ◽  
South Eastern ◽  
Outburst Floods ◽  
Glacial Lake Outburst Floods ◽  
Valley Fills ◽  
Eastern Norway

scholarly journals Simulation and Assessment of Future Glacial Lake Outburst Floods in the Poiqu River Basin, Central Himalayas

Water ◽  
2021 ◽  
Vol 13 (10) ◽  
pp. 1376
Author(s):  
Taigang Zhang ◽  
Weicai Wang ◽  
Tanguang Gao ◽  
Baosheng An
Keyword(s):  
River Basin ◽  
Hazard Assessment ◽  
Glacial Lake ◽  
High Mountain ◽  
Glacial Lakes ◽  
Central Himalayas ◽  
Outburst Floods ◽  
Glacial Lake Outburst Floods ◽  
Social And Economic Development ◽  
Glacial Lake Outburst Flood

A glacial lake outburst flood (GLOF) is a typical glacier-related hazard in high mountain regions. In recent decades, glacial lakes in the Himalayas have expanded rapidly due to climate warming and glacial retreat. Some of these lakes are unstable, and may suddenly burst under different triggering factors, thus draining large amounts of water and impacting downstream social and economic development. Glacial lakes in the Poiqu River basin, Central Himalayas, have attracted great attention since GLOFs originating there could have a transboundary impact on both China and Nepal, as occurred during the Cirenmaco GLOF in 1981 and the Gongbatongshaco GLOF in 2016. Based on previous studies of this basin, we selected seven very high-risk moraine-dammed lakes (Gangxico, Galongco, Jialongco, Cirenmaco, Taraco, Beihu, and Cawuqudenco) to simulate GLOF propagation at different drainage percentage scenarios (i.e., 25%, 50%, 75%, and 100%), and to conduct hazard assessment. The results show that, when any glacial lake is drained completely or partly, most of the floods will enter Nepal after raging in China, and will continue to cause damage. In summary, 57.5 km of roads, 754 buildings, 3.3 km2 of farmland, and 25 bridges are at risk of damage due to GLOFs. The potentially inundated area within the Chinese part of the Poiqu River basin exceeds 45 km2. Due to the destructive impacts of GLOFs on downstream areas, appropriate and effective measures should be implemented to adapt to GLOF risk. We finally present a paradigm for conducting hazard assessment and risk management. It uses only freely available data and thus is easy to apply.

Debris Flows Resulting From Glacial-Lake Outburst Floods in Tibet, China

2010 ◽  
Vol 31 (6) ◽  
pp. 508-527 ◽  
Author(s):  
Peng Cui ◽  
Chao Dang ◽  
Zunlan Cheng ◽  
Kevin M. Scott
Keyword(s):  
Debris Flows ◽  
Glacial Lake ◽  
Outburst Floods ◽  
Glacial Lake Outburst Floods

Landslides in moraines as triggers of glacial lake outburst floods: example from Palcacocha Lake (Cordillera Blanca, Peru)

Landslides ◽  
2016 ◽  
Vol 13 (6) ◽  
pp. 1461-1477 ◽  
Author(s):  
J. Klimeš ◽  
J. Novotný ◽  
I. Novotná ◽  
B. Jordán de Urries ◽  
V. Vilímek ◽  
...  
Keyword(s):  
Glacial Lake ◽  
Cordillera Blanca ◽  
Outburst Floods ◽  
Glacial Lake Outburst Floods

scholarly journals Using satellite images to monitor glacial-lake outburst floods: Lago Cachet Dos drainage, Chile

2015 ◽  
Author(s):  
Beverly A. Friesen ◽  
Christopher J. Cole ◽  
David A. Nimick ◽  
Earl M. Wilson ◽  
Mark J. Fahey ◽  
...  
Keyword(s):  
Satellite Images ◽  
Glacial Lake ◽  
Outburst Floods ◽  
Glacial Lake Outburst Floods

What’s in a lake? Glacial Lake Outburst Floods in the Peruvian Andes.

2021 ◽  
Author(s):  
Joanne Wood ◽  
Stephan Harrison ◽  
Ryan Wilson ◽  
Neil Glasser ◽  
John Reynolds ◽  
...  
Keyword(s):  
Climate Change ◽  
Glacial Lake ◽  
Peruvian Andes ◽  
The Past ◽  
The Andes ◽  
Glacier Recession ◽  
Outburst Floods ◽  
Glacial Lake Outburst Floods ◽  
Lake Systems ◽  
Physical Components

<p>Climate change is resulting in mass loss and the retreat of glaciers in the Andes, exposing steep valley sides, over-deepened valley bottoms, and creating glacial lakes behind moraine dams. Glacial Lake Outburst Floods (GLOFs) present the biggest risk posed by glacier recession in Peru. Understanding the characteristics of lakes that have failed in the past will provide an aid to identifying those lakes that might fail in the future and narrow down which lakes are of greatest interest for reducing the risks to local vulnerable populations. </p><p>Using a newly created lake inventory for the Peruvian Andes (Wood et al., in review) and a comprehensive GLOF inventory (unpublished) we investigate lakes from which GLOFs have occurred in the past. This is to establish which physical components of the glacial lake systems are common to those lakes that have failed previously and which can be identified remotely, easily and objectively, in order to improve existing methods of hazard assessment.</p>

scholarly journals Reconstructing the History of Glacial Lake Outburst Floods (GLOF) in the Kanchenjunga Conservation Area, East Nepal: An Interdisciplinary Approach

2020 ◽  
Vol 12 (13) ◽  
pp. 5407
Author(s):  
Alton C. Byers ◽  
Mohan Bahadur Chand ◽  
Jonathan Lala ◽  
Milan Shrestha ◽  
Elizabeth A. Byers ◽  
...  
Keyword(s):  
Interdisciplinary Approach ◽  
Debris Avalanche ◽  
Field Investigation ◽  
Glacial Lake ◽  
High Mountain ◽  
Lateral Moraine ◽  
Conservation Area ◽  
Terminal Moraine ◽  
Outburst Floods ◽  
Glacial Lake Outburst Floods

An interdisciplinary field investigation of historic glacial lake outburst floods (GLOFs) in the Kanchenjunga region of Nepal was conducted between April and May, 2019. Oral history and field measurements suggested that at least six major GLOFs have occurred in the region since 1921. A remote sensing analysis confirmed the occurrence of the six GLOFs mentioned by informants, including two smaller flood events not mentioned that had occurred at some point before 1962. A numerical simulation of the Nangama GLOF suggested that it was triggered by an ice/debris avalanche of some 800,000 m3 of material, causing a surge wave that breached the terminal moraine and released an estimated 11.2 × 106 m3 ± 1.4 × 106 m3 of water. Debris from the flood dammed the Pabuk Khola river 2 km below the lake to form what is today known as Chheche Pokhari lake. Some concern has been expressed for the possibility of a second GLOF from Nangama as the result of continued and growing landslide activity from its right lateral moraine. Regular monitoring of all lakes and glaciers is recommended to avoid and/or mitigate the occurrence of future GLOF events in the region. Collectively, the paper demonstrates the benefits and utility of interdisciplinary research approaches to achieving a better understanding of past and poorly documented GLOF events in remote, data-scarce high mountain environments.

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