FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4200059956> ?p ?o ?g. }

• W4200059956 abstract "Glaciers across the Himalayan arc are showing varying signs of recession. Glaciers in the eastern and western parts of the Himalayan arc are retreating more rapidly as compared to other regions. This differential retreat is often attributed to climatic, topographic, and geologic influences. The glaciers in the Trans-Himalayan region of Ladakh are believed to be relatively stable as compared to other parts of the western Himalaya. The present study ascertained the area changes and frontal retreat of 87 glaciers in the Pangong Region between 1990 and 2019 using satellite data. The geodetic mass changes were also assessed using SRTM and TanDEM-X digital elevation models of 2000 and 2012 respectively. Besides, the glacier outlines were delineated manually and compared with existing regional and global glacier inventories that are available over the region. The GlabTop model was used to simulate the glacier-bed overdeepenings of four glaciers that are associated with a proglacial lake. The study also analyzed the impact of topographic influences and varying debris cover on glacier recession. This analysis indicated deglaciation of 6.7 ± 0.1% (0.23% a −1 ) from 1990 to 2019 over the Pangong Region with clean-ice glaciers showing a higher retreat (8.4 ± 0.28%) compared to the debris-covered glaciers (5.7 ± 0.14%). However, the overall recession is lower compared to other parts of northwestern Himalayas. The glacier recession showed a positive correlation with mean glacier slope (r = 0.3) and debris cover (r = 0.1) with bigger size glaciers having retreated at a lesser pace compared to smaller ones. This underpins the need for in-situ data about debris thickness to precisely ascertain the role of debris on glacier recession in the Trans-Himalayan Ladakh where debris thickness data is absent. The mean glacier elevation did not indicate any influence on glacier recession. From 2000 to 12, the glaciers lost an ice mass amounting to 0.33 ± 0.05 m we. per year. The formation of four new proglacial lakes, although small (&lt;6 ha), need to be monitored using remote sensing data while the infrastructure development activities should not be permitted given glacial lake outburst flood risk." @default.
• W4200059956 created "2021-12-31" @default.
• W4200059956 creator A5006470697 @default.
• W4200059956 creator A5012608325 @default.
• W4200059956 creator A5043736721 @default.
• W4200059956 creator A5075760451 @default.
• W4200059956 date "2021-12-23" @default.
• W4200059956 modified "2023-10-18" @default.
• W4200059956 title "Spatiotemporal Dynamics and Geodetic Mass Changes of Glaciers With Varying Debris Cover in the Pangong Region of Trans-Himalayan Ladakh, India Between 1990 and 2019" @default.
• W4200059956 cites W1544860600 @default.
• W4200059956 cites W1967220287 @default.
• W4200059956 cites W1973200177 @default.
• W4200059956 cites W1973765414 @default.
• W4200059956 cites W1987967699 @default.
• W4200059956 cites W2016250055 @default.
• W4200059956 cites W2018369970 @default.
• W4200059956 cites W2019916967 @default.
• W4200059956 cites W2024695456 @default.
• W4200059956 cites W2026018392 @default.
• W4200059956 cites W2029153117 @default.
• W4200059956 cites W2031044308 @default.
• W4200059956 cites W2031494969 @default.
• W4200059956 cites W2039255978 @default.
• W4200059956 cites W2040953565 @default.
• W4200059956 cites W2046508775 @default.
• W4200059956 cites W2059799756 @default.
• W4200059956 cites W2066907097 @default.
• W4200059956 cites W2067952092 @default.
• W4200059956 cites W2068323264 @default.
• W4200059956 cites W2080584583 @default.
• W4200059956 cites W2085585287 @default.
• W4200059956 cites W2089460721 @default.
• W4200059956 cites W2093936554 @default.
• W4200059956 cites W2119284220 @default.
• W4200059956 cites W2124652916 @default.
• W4200059956 cites W2136111517 @default.
• W4200059956 cites W2150337006 @default.
• W4200059956 cites W2156661232 @default.
• W4200059956 cites W2156678124 @default.
• W4200059956 cites W2164865271 @default.
• W4200059956 cites W2168601869 @default.
• W4200059956 cites W2173076085 @default.
• W4200059956 cites W2193890681 @default.
• W4200059956 cites W2289313402 @default.
• W4200059956 cites W2344976613 @default.
• W4200059956 cites W2404463793 @default.
• W4200059956 cites W2522546486 @default.
• W4200059956 cites W2550521585 @default.
• W4200059956 cites W2584693384 @default.
• W4200059956 cites W2589218459 @default.
• W4200059956 cites W2606639769 @default.
• W4200059956 cites W2615177226 @default.
• W4200059956 cites W2734386147 @default.
• W4200059956 cites W2756928373 @default.
• W4200059956 cites W2766037940 @default.
• W4200059956 cites W2783298993 @default.
• W4200059956 cites W2792134378 @default.
• W4200059956 cites W2793809855 @default.
• W4200059956 cites W2794989712 @default.
• W4200059956 cites W2795570725 @default.
• W4200059956 cites W2796752115 @default.
• W4200059956 cites W2803904041 @default.
• W4200059956 cites W2809135700 @default.
• W4200059956 cites W2840190924 @default.
• W4200059956 cites W2901296248 @default.
• W4200059956 cites W2907753745 @default.
• W4200059956 cites W2910209285 @default.
• W4200059956 cites W2913406739 @default.
• W4200059956 cites W2916558994 @default.
• W4200059956 cites W2921014872 @default.
• W4200059956 cites W2921547444 @default.
• W4200059956 cites W2924528214 @default.
• W4200059956 cites W2941830643 @default.
• W4200059956 cites W2944190788 @default.
• W4200059956 cites W2946817219 @default.
• W4200059956 cites W2950929975 @default.
• W4200059956 cites W2965738081 @default.
• W4200059956 cites W2972386534 @default.
• W4200059956 cites W2981781315 @default.
• W4200059956 cites W2986991701 @default.
• W4200059956 cites W3007409653 @default.
• W4200059956 cites W3007427494 @default.
• W4200059956 cites W3023034143 @default.
• W4200059956 cites W3028150977 @default.
• W4200059956 cites W3032984267 @default.
• W4200059956 cites W3042448204 @default.
• W4200059956 cites W3044088756 @default.
• W4200059956 cites W3045763914 @default.
• W4200059956 cites W3061415658 @default.
• W4200059956 cites W3082335603 @default.
• W4200059956 cites W3083104363 @default.
• W4200059956 cites W3086066135 @default.
• W4200059956 cites W3096975521 @default.
• W4200059956 cites W3104715597 @default.
• W4200059956 cites W3108181270 @default.
• W4200059956 cites W3137297106 @default.
• W4200059956 cites W3141715430 @default.
• W4200059956 cites W3157736499 @default.
• W4200059956 cites W3166648790 @default.
• W4200059956 cites W3180447170 @default.

• next