Spatio-temporal assessment of areal fragmentation and volume of snow cover in the central Himalaya

Assigned Session: FS 3.116: High mountain hydrology and cryosphere under global change: observations, modelling, prospects

Abstract ID: 3.8250 | Pending | Talk/Oral | TBA | TBA

Surajit Banerjee (0)
Sati, Vishwambhar Prasad (1)
Surajit Banerjee ((0) Mizoram University, Mizoram University Road, 796004, Aizawl, Mizoram, IN)
Sati, Vishwambhar Prasad (1)

(0) Mizoram University, Mizoram University Road, 796004, Aizawl, Mizoram, IN
(1) Mizoram University, Mizoram University Road, 796004, Aizawl, Mizoram, India

(1) Mizoram University, Mizoram University Road, 796004, Aizawl, Mizoram, India

Categories: Cryo- & Hydrosphere, Low-to-no-snow, Remote Sensing
Keywords: Snow cover dynamics, Glacier, Central Himalayas, Snow cover fragmentation, Landscape metrics

Categories: Cryo- & Hydrosphere, Low-to-no-snow, Remote Sensing
Keywords: Snow cover dynamics, Glacier, Central Himalayas, Snow cover fragmentation, Landscape metrics

The content was (partly) adapted by AI
Content (partly) adapted by AI

Central Himalaya, the third-largest ice mass globally, is the source of major rivers like the Ganges, upon which almost 655 million people from India, Nepal, and Bangladesh rely for livelihood. However, climate change is the largest threat to its snow cover. Therefore, this study utilizes remotely sensed data to examine spatio-temporal variations in snow cover area, volume, and areal fragmentation over thirty years. Different landscape metrics (class area, number of patches, patch density, largest patch index, mean patch size, edge density, and perimeter area ratio) are used and a novel index is developed to study fragmentation. NDSI is used to map the snow cover and area volume scaling based on empirical observations to estimate the volume. Despite fluctuations, a trend of decline emerges in thick and thin snow cover (from 10768 km² to 3258.6 km² in thick snow, and from 3798 km² to 6863.56 km² in thin snow during maxima, whereas, from 1678.44 km² to 539.66 km² in thick snow and from 2414.12 km² to 1300.56 km² in thin snow during minima). Thick snow cover fluctuated with a period of decline up to 2006, followed by a slight recovery and subsequent reduction in 2021. Conversely, thin snow cover shows a gradual increase up to 2006, followed by a rapid decline in 2021, highlighting the region’s high susceptibility to warming. Furthermore, it was found that B4, C2, C3, and C4 were the grids with very high fragmentation of thick snow. However, C1, D2, and E4 were marked as highly fragmented for thin snow cover. The research underscores the urgent need for adaptive and mitigation measures to impact climate change in the fragile cryosphere of the Central Himalayas.


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