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Strengthening Water Resources Management in
Afghanistan (SWaRMA)
Training Workshop on Multi-scale Integrated River Basin Management from a HKH perspective
GLOF Risk Reduction
Finu Shrestha, Sharad Joshi, Anna Sinisalo
Glacial lake
Lake
Glacial lake is formed as the result of glacier melt/shrink,
which often left behind large debris deposits
Lakes may be formed either within part of the eroded
landform (e.g. bed rock dammed) or build behind a dam
formed by moraines, ice and/or landslide debris
Glacial lakes are not only the important refresh water resources, but also
act as a trigger of many glacial hazards such as glacial lake outburst flood
(GLOF) and debris flow
Glacial lake outburst flood (GLOF)
When the natural dam fails
Failure can happen due to erosion, seepage, a buildup of water
pressure, rock fall, ice or large snow avalanche and an earthquake
Past GLOF events in Nepal
Dig Tsho GLOF event of 1985 Chhukung village downstream of Imja TshoDudh Koshi below Imja lake showing remains of
damage from the 1977 Nare GLOF
Photo: Sharad P. Joshi
• Glacial lake inventory
• Monitoring of potentially dangerous glacial lakes
• GLOF risk knowledge (Triggering factors to GLOF)
• Risk assessment (GLOF hazard and vulnerability mapping)
• Early warning system (EWS)
• Mitigation measures
• Capacity building and training
• Public awareness and education
• Emergency preparedness and response
• Transboundary GLOF issues
• Regulation and enforcement
How risk is reduced?
Community involvement
Early warning systems (EWS))
The transmitter station of
Sangma Kharka outside Tsho
Rolpa Lake receives signals
from sensors and transmits to
other remote warning stations
GLOF Sensor and early warning
system in the Bhote Koshi,
(a) Sensor at River Level,
(b) Sensor at Friendship Bridge,
(c) Early warning system siren
Case studies (Tsho Rolpa & Bhote Koshi in Nepal)
Siphon across the end moraine
Mitigation measures of Tsho Rolpa glacial lake to reduce
its water level
Moraine-dammed lake with
a natural spillway (left) and
an artificial outlet (right)
Mitigation measures being
implemented at the end
moraine
Construction of the outlet
canal and gates
Mitigation measures
Tsho Rolpa Lake in Nepal
Outlet canal with gated structure to drain water at Tsho Rolpa Glacial Lake
Mitigation measures
• Awareness raising programmes
• Participate in the exercises and rehearsal of emergency plan &
programmes.
• Community leaders should be trained
• Put communities in charge of early warning
Community participation in risk reduction
Example: Tsho Rolpa Glacial Lake
Tsho Rolpa glacial lake Nov 1994 (SPJ) Tsho Rolpa glacial lake Nov 2018 (G.Earth)
GLOF in Panjshir Province, Afghanistan
12 July, 2018
Field photographs showing the crack in the
moraine dam at lake snout and remnant of the
lake after breach. Source: MEW
Pleiades image (0.5m ) from 19 July, 2018. Black boundary shows the crack in the moraine dam at
lake snout and blue boundary shows the lake area before the breach
Group Work!
Group Work!
Imja Lake Mitigation, 2016
Bhutan: Lake Mitigation
Atro Sar Lake
Group work
Is a lake dangerous?
If No, Why?
If Yes, what are the triggering factors for
GLOF?
What can be done to GLOF Risk
reduction?
RIVER BASINS & CRYOSPHERE 23
Thank you

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Strengthening Water Resource Management and Reducing GLOF Risk in Afghanistan

  • 1. Strengthening Water Resources Management in Afghanistan (SWaRMA) Training Workshop on Multi-scale Integrated River Basin Management from a HKH perspective GLOF Risk Reduction Finu Shrestha, Sharad Joshi, Anna Sinisalo
  • 2. Glacial lake Lake Glacial lake is formed as the result of glacier melt/shrink, which often left behind large debris deposits Lakes may be formed either within part of the eroded landform (e.g. bed rock dammed) or build behind a dam formed by moraines, ice and/or landslide debris Glacial lakes are not only the important refresh water resources, but also act as a trigger of many glacial hazards such as glacial lake outburst flood (GLOF) and debris flow
  • 3. Glacial lake outburst flood (GLOF) When the natural dam fails Failure can happen due to erosion, seepage, a buildup of water pressure, rock fall, ice or large snow avalanche and an earthquake
  • 4. Past GLOF events in Nepal Dig Tsho GLOF event of 1985 Chhukung village downstream of Imja TshoDudh Koshi below Imja lake showing remains of damage from the 1977 Nare GLOF Photo: Sharad P. Joshi
  • 5. • Glacial lake inventory • Monitoring of potentially dangerous glacial lakes • GLOF risk knowledge (Triggering factors to GLOF) • Risk assessment (GLOF hazard and vulnerability mapping) • Early warning system (EWS) • Mitigation measures • Capacity building and training • Public awareness and education • Emergency preparedness and response • Transboundary GLOF issues • Regulation and enforcement How risk is reduced? Community involvement
  • 6. Early warning systems (EWS)) The transmitter station of Sangma Kharka outside Tsho Rolpa Lake receives signals from sensors and transmits to other remote warning stations GLOF Sensor and early warning system in the Bhote Koshi, (a) Sensor at River Level, (b) Sensor at Friendship Bridge, (c) Early warning system siren Case studies (Tsho Rolpa & Bhote Koshi in Nepal)
  • 7. Siphon across the end moraine Mitigation measures of Tsho Rolpa glacial lake to reduce its water level Moraine-dammed lake with a natural spillway (left) and an artificial outlet (right) Mitigation measures being implemented at the end moraine Construction of the outlet canal and gates Mitigation measures Tsho Rolpa Lake in Nepal
  • 8. Outlet canal with gated structure to drain water at Tsho Rolpa Glacial Lake Mitigation measures
  • 9. • Awareness raising programmes • Participate in the exercises and rehearsal of emergency plan & programmes. • Community leaders should be trained • Put communities in charge of early warning Community participation in risk reduction
  • 10. Example: Tsho Rolpa Glacial Lake Tsho Rolpa glacial lake Nov 1994 (SPJ) Tsho Rolpa glacial lake Nov 2018 (G.Earth)
  • 11.
  • 12. GLOF in Panjshir Province, Afghanistan 12 July, 2018
  • 13. Field photographs showing the crack in the moraine dam at lake snout and remnant of the lake after breach. Source: MEW Pleiades image (0.5m ) from 19 July, 2018. Black boundary shows the crack in the moraine dam at lake snout and blue boundary shows the lake area before the breach
  • 18.
  • 19.
  • 20.
  • 21. Group work Is a lake dangerous? If No, Why? If Yes, what are the triggering factors for GLOF? What can be done to GLOF Risk reduction?
  • 22.
  • 23. RIVER BASINS & CRYOSPHERE 23 Thank you