Glacial lake outburst flood risk assessment of a rapidly expanding glacial lake in the Ladakh region of Western Himalaya, using hydrodynamic modeling DOI Creative Commons

Abid Farooq Rather,

Rayees Ahmed, Joshal Kumar Bansal

и другие.

Geomatics Natural Hazards and Risk, Год журнала: 2024, Номер 15(1)

Опубликована: Окт. 21, 2024

The ongoing trend of warming climate has made Glacial Lake Outburst Floods (GLOFs) a major cryospheric hazard worldwide, especially in the Himalayas. GLOFs Himalayan region are mostly caused by moraine-dammed proglacial lakes and ice-dammed lakes. These sporadic disasters have resulted significant loss life property. This study offers comprehensive analysis GLOF potential potentially dangerous lake (PDGL) Ladakh region. research explores threat from using multi-criteria advanced 2D hydrodynamic modeling approaches. mass balance response mother glacier, its flow dynamics, glacier-lake interactions were examined for past 22 years. findings show that over this period, PDGL had notable expansion 78.7%, accompanied recession 13.2% feeding glacier. glacier witnessed an average thickness ⁓7 m at rate 0.32 a−1 during period. average, lowest, maximum depth found to be 30.95, 14.30, 50.57 m, respectively velocity was estimated as 3.38 a−1. Because lake's rapid steep surrounding slopes, it classified high-hazard lake. risk downstream community assessed through HEC-RAS tool. discharge under worst-case scenario piping overtopping failures 3890.99 m3s−1 5111.39 m3s−1, respectively. area inundation calculated 4.74 5.38 km2 moderate scenarios expected flood velocities range 18.26 23.78 meters, scenarios. At several locations area, routed hydrographs representing propagation generated. wave would arrive first settlement 50 min, with peak 12.36 s−1. inundated includes critical infrastructure such bridges, residential houses, roads. To mitigate associated lake, more detailed on-site is highly recommended.

Язык: Английский

Time to diffuse the “ticking time bombs” of the Himalaya DOI Creative Commons
Anshuman Bhardwaj, Sheikh Nawaz Ali, Lydia Sam

и другие.

Physics and Chemistry of the Earth Parts A/B/C, Год журнала: 2025, Номер unknown, С. 103908 - 103908

Опубликована: Март 1, 2025

Язык: Английский

Процитировано

1

Multidisciplinary Perspectives in Understanding Himalayan glacial lakes in a Climate Challenged World DOI Creative Commons
Nitesh Khadka, Weiming Liu, Milan Shrestha

и другие.

Опубликована: Фев. 1, 2025

Язык: Английский

Процитировано

0

Multi Breach GLOF Hazard and Exposure Analysis of Birendra Lake in the Manaslu Region of Nepal DOI Creative Commons
Utsav Poudel, Manish Raj Gouli, Kaiheng Hu

и другие.

Natural Hazards Research, Год журнала: 2025, Номер unknown

Опубликована: Март 1, 2025

Язык: Английский

Процитировано

0

Glacial lake outburst floods (GLOFs): causes, modeling, and mitigation in Indian Himalayan region DOI
Sharad K. Jain, Sanjay K. Jain,

Rayees Ahmad

и другие.

GeoJournal, Год журнала: 2025, Номер 90(2)

Опубликована: Апрель 9, 2025

Язык: Английский

Процитировано

0

Glacial lake outburst flood risk assessment of a rapidly expanding glacial lake in the Ladakh region of Western Himalaya, using hydrodynamic modeling DOI Creative Commons

Abid Farooq Rather,

Rayees Ahmed, Joshal Kumar Bansal

и другие.

Geomatics Natural Hazards and Risk, Год журнала: 2024, Номер 15(1)

Опубликована: Окт. 21, 2024

The ongoing trend of warming climate has made Glacial Lake Outburst Floods (GLOFs) a major cryospheric hazard worldwide, especially in the Himalayas. GLOFs Himalayan region are mostly caused by moraine-dammed proglacial lakes and ice-dammed lakes. These sporadic disasters have resulted significant loss life property. This study offers comprehensive analysis GLOF potential potentially dangerous lake (PDGL) Ladakh region. research explores threat from using multi-criteria advanced 2D hydrodynamic modeling approaches. mass balance response mother glacier, its flow dynamics, glacier-lake interactions were examined for past 22 years. findings show that over this period, PDGL had notable expansion 78.7%, accompanied recession 13.2% feeding glacier. glacier witnessed an average thickness ⁓7 m at rate 0.32 a−1 during period. average, lowest, maximum depth found to be 30.95, 14.30, 50.57 m, respectively velocity was estimated as 3.38 a−1. Because lake's rapid steep surrounding slopes, it classified high-hazard lake. risk downstream community assessed through HEC-RAS tool. discharge under worst-case scenario piping overtopping failures 3890.99 m3s−1 5111.39 m3s−1, respectively. area inundation calculated 4.74 5.38 km2 moderate scenarios expected flood velocities range 18.26 23.78 meters, scenarios. At several locations area, routed hydrographs representing propagation generated. wave would arrive first settlement 50 min, with peak 12.36 s−1. inundated includes critical infrastructure such bridges, residential houses, roads. To mitigate associated lake, more detailed on-site is highly recommended.

Язык: Английский

Процитировано

1