FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2803904041> ?p ?o ?g. }

• W2803904041 endingPage "396" @default.
• W2803904041 startingPage "376" @default.
• W2803904041 abstract "Glacier recession and formation of glacial lakes along with outburst flood hazards are increasing in response to changing climate in the Himalayan region. This study describes evolution of Dalung and Padam glaciers and their associated lakes employing multi-temporal datasets of Landsat (MSS, TM, ETM+), Indian Remote Sensing LISS-III, Google EarthTM, ASTER GDEM and Survey of India topographic maps. The Dalung Glacier (DG) and Lake (DL) are present in Suru River catchment whereas the Padam Glacier (PG) and Lake (PL) are present in Tsarap River catchment of Zanskar basin, western Himalaya. From 1962 to 2015; the DG and PG have shrunk at different rates. The DG has shrunk by 2.6 ± 0.56 km2 (19.2 ± 4.1%) at a rate of 0.05 ± 0.01 km2 a−1 whereas, the PG has shrunk by 3.4 ± 0.65 km2 (12.7 ± 2.4%) at a rate of 0.06 ± 0.01 km2 a−1. The frontal recession was recorded as 1.240 ± 0.02 km (15.7 ± 2.0%) at a rate of 20 ± 0.4 m a−1 for DG and 2.690 ± 0.5 m (21.3 ± 2.1%) at a rate of 50.7 ± 0.1 m a−1 for PG. Consequently, the proglacial glacial lakes have formed indicating an expansion of 20 ± 3.4% (DL) and 58 ± 4.5% (PL) during 1990–2015. Using integrated criteria of standard indices for the identification of potentially dangerous glacial lakes (PDGLs), the lakes were found to be vulnerable and have a potential to cause breaching in the coming years. In order to provide inputs for the emergency action plan, one dimensional MIKE 11 Model was used to generate the peak flood hydrographs at the lake and other vulnerable sites downstream. Highest peak discharge of 3361.7 m3 s−1 (DL) and 4210.3 m3 s−1 (PL) were estimated at the lake sites which has reduced to 1520.9 m3 s−1 and 1722.4 m3 s−1 respectively at the outlet sites. The reduced discharge at downstream sites still bears the potential to create dangerous flood hazards." @default.
• W2803904041 created "2018-06-01" @default.
• W2803904041 creator A5031834040 @default.
• W2803904041 creator A5054072948 @default.
• W2803904041 creator A5070808070 @default.
• W2803904041 creator A5084677743 @default.
• W2803904041 date "2018-09-01" @default.
• W2803904041 modified "2023-10-16" @default.
• W2803904041 title "Glacier recession and glacial lake outburst flood studies in Zanskar basin, western Himalaya" @default.
• W2803904041 cites W102823611 @default.
• W2803904041 cites W130987747 @default.
• W2803904041 cites W1489943945 @default.
• W2803904041 cites W1671654396 @default.
• W2803904041 cites W1857372911 @default.
• W2803904041 cites W1961672453 @default.
• W2803904041 cites W1964749110 @default.
• W2803904041 cites W1965270923 @default.
• W2803904041 cites W1966180238 @default.
• W2803904041 cites W1968408909 @default.
• W2803904041 cites W1968580830 @default.
• W2803904041 cites W1969742994 @default.
• W2803904041 cites W1971257088 @default.
• W2803904041 cites W1971400458 @default.
• W2803904041 cites W1973200177 @default.
• W2803904041 cites W1975117422 @default.
• W2803904041 cites W1975539638 @default.
• W2803904041 cites W1975916482 @default.
• W2803904041 cites W1976700493 @default.
• W2803904041 cites W1978358208 @default.
• W2803904041 cites W1979670443 @default.
• W2803904041 cites W1981005461 @default.
• W2803904041 cites W1982526103 @default.
• W2803904041 cites W1984576625 @default.
• W2803904041 cites W1984931425 @default.
• W2803904041 cites W1989695705 @default.
• W2803904041 cites W1992098736 @default.
• W2803904041 cites W1996766450 @default.
• W2803904041 cites W1996862175 @default.
• W2803904041 cites W2004459073 @default.
• W2803904041 cites W2004853484 @default.
• W2803904041 cites W2006508734 @default.
• W2803904041 cites W2006919898 @default.
• W2803904041 cites W2011220026 @default.
• W2803904041 cites W2014693698 @default.
• W2803904041 cites W2016502779 @default.
• W2803904041 cites W2020143766 @default.
• W2803904041 cites W2023593473 @default.
• W2803904041 cites W2024695456 @default.
• W2803904041 cites W2031044308 @default.
• W2803904041 cites W2031507317 @default.
• W2803904041 cites W2031700439 @default.
• W2803904041 cites W2035739819 @default.
• W2803904041 cites W2039255978 @default.
• W2803904041 cites W2041369670 @default.
• W2803904041 cites W2044145323 @default.
• W2803904041 cites W2045908416 @default.
• W2803904041 cites W2045927713 @default.
• W2803904041 cites W2046406789 @default.
• W2803904041 cites W2047451958 @default.
• W2803904041 cites W2047694522 @default.
• W2803904041 cites W2059891119 @default.
• W2803904041 cites W2062391457 @default.
• W2803904041 cites W2063684593 @default.
• W2803904041 cites W2063794916 @default.
• W2803904041 cites W2066144694 @default.
• W2803904041 cites W2066907097 @default.
• W2803904041 cites W2070359395 @default.
• W2803904041 cites W2072519407 @default.
• W2803904041 cites W2073771362 @default.
• W2803904041 cites W2074828457 @default.
• W2803904041 cites W2077020350 @default.
• W2803904041 cites W2079714625 @default.
• W2803904041 cites W2080058134 @default.
• W2803904041 cites W2085683568 @default.
• W2803904041 cites W2086139388 @default.
• W2803904041 cites W2086620533 @default.
• W2803904041 cites W2088683137 @default.
• W2803904041 cites W2089617377 @default.
• W2803904041 cites W2093936554 @default.
• W2803904041 cites W2100046288 @default.
• W2803904041 cites W2101490545 @default.
• W2803904041 cites W2106839269 @default.
• W2803904041 cites W2117706739 @default.
• W2803904041 cites W2126411775 @default.
• W2803904041 cites W2126453327 @default.
• W2803904041 cites W2128202857 @default.
• W2803904041 cites W2128311680 @default.
• W2803904041 cites W2131176650 @default.
• W2803904041 cites W2137746318 @default.
• W2803904041 cites W2138244549 @default.
• W2803904041 cites W2139344841 @default.
• W2803904041 cites W2140490114 @default.
• W2803904041 cites W2143523928 @default.
• W2803904041 cites W2144405045 @default.
• W2803904041 cites W2145791900 @default.
• W2803904041 cites W2151022888 @default.
• W2803904041 cites W2156678124 @default.
• W2803904041 cites W2163969318 @default.

• next