Matches in SemOpenAlex for { <https://semopenalex.org/work/W3025502403> ?p ?o ?g. }
- W3025502403 endingPage "1563" @default.
- W3025502403 startingPage "1563" @default.
- W3025502403 abstract "Meltwater from the glaciers in High Mountain Asia plays a critical role in water availability and food security in central and southern Asia. However, observations of glacier ablation and accumulation rates are limited in spatial and temporal scale due to the challenges that are associated with fieldwork at the remote, high-altitude settings of these glaciers. Here, using a remote-sensing-based mass-continuity approach, we compute regional-scale surface mass balance of glaciers in five key regions across High Mountain Asia. After accounting for the role of ice flow, we find distinctively different altitudinal surface-mass-balance gradients between heavily debris-covered and relatively debris-free areas. In the region surrounding Mount Everest, where debris coverage is the most extensive, our results show a reversed mean surface-mass-balance gradient of −0.21 ± 0.18 m w.e. a−1 (100 m)−1 on the low-elevation portions of glaciers, switching to a positive mean gradient of 1.21 ± 0.41 m w.e. a−1 (100 m)−1 above an average elevation of 5520 ± 50 m. Meanwhile, in West Nepal, where the debris coverage is minimal, we find a continuously positive mean gradient of 1.18 ± 0.40 m w.e. a−1 (100 m)−1. Equilibrium line altitude estimates, which are derived from our surface-mass-balance gradients, display a strong regional gradient, increasing from northwest (4490 ± 140 m) to southeast (5690 ± 130 m). Overall, our findings emphasise the importance of separating signals of surface mass balance and ice dynamics, in order to constrain better their contribution towards the ice thinning that is being observed across High Mountain Asia." @default.
- W3025502403 created "2020-05-21" @default.
- W3025502403 creator A5004111894 @default.
- W3025502403 creator A5024755265 @default.
- W3025502403 creator A5030625710 @default.
- W3025502403 creator A5035617065 @default.
- W3025502403 creator A5057329581 @default.
- W3025502403 creator A5060411175 @default.
- W3025502403 date "2020-05-14" @default.
- W3025502403 modified "2023-10-05" @default.
- W3025502403 title "Reversed Surface-Mass-Balance Gradients on Himalayan Debris-Covered Glaciers Inferred from Remote Sensing" @default.
- W3025502403 cites W1492998885 @default.
- W3025502403 cites W1832320792 @default.
- W3025502403 cites W1973200177 @default.
- W3025502403 cites W1977033525 @default.
- W3025502403 cites W1984576625 @default.
- W3025502403 cites W1991093099 @default.
- W3025502403 cites W1994869682 @default.
- W3025502403 cites W1997764658 @default.
- W3025502403 cites W1999516172 @default.
- W3025502403 cites W2001071094 @default.
- W3025502403 cites W2018214942 @default.
- W3025502403 cites W2050056252 @default.
- W3025502403 cites W2076732188 @default.
- W3025502403 cites W2084744129 @default.
- W3025502403 cites W2092369902 @default.
- W3025502403 cites W2093936554 @default.
- W3025502403 cites W2106944596 @default.
- W3025502403 cites W2110091130 @default.
- W3025502403 cites W2141169867 @default.
- W3025502403 cites W2150022032 @default.
- W3025502403 cites W2165092456 @default.
- W3025502403 cites W2167268384 @default.
- W3025502403 cites W2170750509 @default.
- W3025502403 cites W2292752936 @default.
- W3025502403 cites W2292938054 @default.
- W3025502403 cites W2323409967 @default.
- W3025502403 cites W2328369642 @default.
- W3025502403 cites W2346364990 @default.
- W3025502403 cites W2399201887 @default.
- W3025502403 cites W2439245909 @default.
- W3025502403 cites W2553825161 @default.
- W3025502403 cites W2726476000 @default.
- W3025502403 cites W2737548698 @default.
- W3025502403 cites W2751889582 @default.
- W3025502403 cites W2755224296 @default.
- W3025502403 cites W2767289157 @default.
- W3025502403 cites W2784513399 @default.
- W3025502403 cites W2802060640 @default.
- W3025502403 cites W2807616569 @default.
- W3025502403 cites W2898442636 @default.
- W3025502403 cites W2899371593 @default.
- W3025502403 cites W2903568952 @default.
- W3025502403 cites W2912817725 @default.
- W3025502403 cites W2922096344 @default.
- W3025502403 cites W2936322338 @default.
- W3025502403 cites W2982016643 @default.
- W3025502403 cites W2996482094 @default.
- W3025502403 cites W2997758357 @default.
- W3025502403 cites W3003669653 @default.
- W3025502403 cites W4210727842 @default.
- W3025502403 doi "https://doi.org/10.3390/rs12101563" @default.
- W3025502403 hasPublicationYear "2020" @default.
- W3025502403 type Work @default.
- W3025502403 sameAs 3025502403 @default.
- W3025502403 citedByCount "27" @default.
- W3025502403 countsByYear W30255024032020 @default.
- W3025502403 countsByYear W30255024032021 @default.
- W3025502403 countsByYear W30255024032022 @default.
- W3025502403 countsByYear W30255024032023 @default.
- W3025502403 crossrefType "journal-article" @default.
- W3025502403 hasAuthorship W3025502403A5004111894 @default.
- W3025502403 hasAuthorship W3025502403A5024755265 @default.
- W3025502403 hasAuthorship W3025502403A5030625710 @default.
- W3025502403 hasAuthorship W3025502403A5035617065 @default.
- W3025502403 hasAuthorship W3025502403A5057329581 @default.
- W3025502403 hasAuthorship W3025502403A5060411175 @default.
- W3025502403 hasBestOaLocation W30255024031 @default.
- W3025502403 hasConcept C100834320 @default.
- W3025502403 hasConcept C100970517 @default.
- W3025502403 hasConcept C111368507 @default.
- W3025502403 hasConcept C114793014 @default.
- W3025502403 hasConcept C121332964 @default.
- W3025502403 hasConcept C127045886 @default.
- W3025502403 hasConcept C127313418 @default.
- W3025502403 hasConcept C1276947 @default.
- W3025502403 hasConcept C136894858 @default.
- W3025502403 hasConcept C171289182 @default.
- W3025502403 hasConcept C193091731 @default.
- W3025502403 hasConcept C197435368 @default.
- W3025502403 hasConcept C205649164 @default.
- W3025502403 hasConcept C207318512 @default.
- W3025502403 hasConcept C2524010 @default.
- W3025502403 hasConcept C2776023875 @default.
- W3025502403 hasConcept C33923547 @default.
- W3025502403 hasConcept C37054046 @default.
- W3025502403 hasConcept C39432304 @default.
- W3025502403 hasConcept C49204034 @default.