FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4384938557> ?p ?o ?g. }

• W4384938557 endingPage "103965" @default.
• W4384938557 startingPage "103965" @default.
• W4384938557 abstract "This study assesses the impact of glacier changes and their effects on glacier melt runoff over three different Himalayan river basins located in western Himalaya (i.e. Baspa and Ganga) and eastern Himalaya (Teesta). For computation of glacier melt runoff, a fully distributed snow-glacier melt runoff model viz. SPHY has been used. The glacier area changes have been computed by preparing the glacier maps for different years for all selected river basins viz. Baspa (for year 2000 & 2018), Ganga (for year 1990, 2000, 2010 and 2020) and Teesta (for year 2000 and 2020). Results showed that the glacier areas have noticeably reduced for all Himalayan river basins viz. Baspa (~19.8%), Ganga (~5.01%) and Teesta (~5%). It has been observed that smaller glaciers have more significantly reduced than large glaciers. The strength of the glacier melt induced runoff computation has been evaluated with reference to observed discharge at different gauges in all selected river basins, which showed a reliable agreement between modeled and observed runoff (R2 > 0.7). To see the behavior of runoff for different glacier sized watersheds, the three basins have been divided into a number of watersheds. In Baspa four watersheds while for Ganga and Teesta basins, six watersheds have finally selected depending on quantum of glacier. As per the decadal computation of glacier melt scenarios for all river basins viz. Baspa (i.e. 2003–2010 and 2011–2018), Ganga (1986–1995, 1996–2005, 2006–2015, and 2011–2020) and Teesta (1996–2010 and 2006–2020), observations showed that watersheds having large glaciers, the melt runoff has increased, while in cases of the watersheds having small glaciers, the melt runoff has decreased due to reduced glacier cover. In case of Baspa basin, glacier melt runoff has decreased by 5% while for Ganga and Teesta basins it has increased by 1%. Similarly, for Baspa basin, snowmelt runoff has increased by 6% and for Ganga and Teesta it has decreased by 3%." @default.
• W4384938557 created "2023-07-22" @default.
• W4384938557 creator A5046840342 @default.
• W4384938557 creator A5054072948 @default.
• W4384938557 creator A5065441437 @default.
• W4384938557 date "2023-10-01" @default.
• W4384938557 modified "2023-09-25" @default.
• W4384938557 title "A comparative analysis of glacier and glacier-melt runoff changes in western and eastern Himalayan river basins" @default.
• W4384938557 cites W1987619581 @default.
• W4384938557 cites W2009463208 @default.
• W4384938557 cites W2026018392 @default.
• W4384938557 cites W2043575985 @default.
• W4384938557 cites W2056909794 @default.
• W4384938557 cites W2057035657 @default.
• W4384938557 cites W2060917378 @default.
• W4384938557 cites W2066907097 @default.
• W4384938557 cites W2095989164 @default.
• W4384938557 cites W2133894646 @default.
• W4384938557 cites W2137446795 @default.
• W4384938557 cites W2141169867 @default.
• W4384938557 cites W2173640817 @default.
• W4384938557 cites W2467909254 @default.
• W4384938557 cites W2519189185 @default.
• W4384938557 cites W2556497429 @default.
• W4384938557 cites W2609150059 @default.
• W4384938557 cites W2616483903 @default.
• W4384938557 cites W2783298993 @default.
• W4384938557 cites W2784513399 @default.
• W4384938557 cites W2799833447 @default.
• W4384938557 cites W2899404378 @default.
• W4384938557 cites W2995675009 @default.
• W4384938557 cites W2999003120 @default.
• W4384938557 cites W3001777192 @default.
• W4384938557 cites W3041038745 @default.
• W4384938557 cites W3046260540 @default.
• W4384938557 cites W3087787106 @default.
• W4384938557 cites W3088236261 @default.
• W4384938557 cites W3117950312 @default.
• W4384938557 cites W3120624109 @default.
• W4384938557 cites W3120767031 @default.
• W4384938557 cites W3122435590 @default.
• W4384938557 cites W3127199302 @default.
• W4384938557 cites W3133270431 @default.
• W4384938557 cites W3150973955 @default.
• W4384938557 cites W3166648790 @default.
• W4384938557 cites W3207186577 @default.
• W4384938557 cites W4200142003 @default.
• W4384938557 cites W4210829661 @default.
• W4384938557 cites W4225500699 @default.
• W4384938557 cites W4367312863 @default.
• W4384938557 doi "https://doi.org/10.1016/j.coldregions.2023.103965" @default.
• W4384938557 hasPublicationYear "2023" @default.
• W4384938557 type Work @default.
• W4384938557 citedByCount "0" @default.
• W4384938557 crossrefType "journal-article" @default.
• W4384938557 hasAuthorship W4384938557A5046840342 @default.
• W4384938557 hasAuthorship W4384938557A5054072948 @default.
• W4384938557 hasAuthorship W4384938557A5065441437 @default.
• W4384938557 hasConcept C100834320 @default.
• W4384938557 hasConcept C100970517 @default.
• W4384938557 hasConcept C104932425 @default.
• W4384938557 hasConcept C114793014 @default.
• W4384938557 hasConcept C126645576 @default.
• W4384938557 hasConcept C127045886 @default.
• W4384938557 hasConcept C127313418 @default.
• W4384938557 hasConcept C136894858 @default.
• W4384938557 hasConcept C187320778 @default.
• W4384938557 hasConcept C18903297 @default.
• W4384938557 hasConcept C193091731 @default.
• W4384938557 hasConcept C197046000 @default.
• W4384938557 hasConcept C197435368 @default.
• W4384938557 hasConcept C205649164 @default.
• W4384938557 hasConcept C49204034 @default.
• W4384938557 hasConcept C50477045 @default.
• W4384938557 hasConcept C58640448 @default.
• W4384938557 hasConcept C76886044 @default.
• W4384938557 hasConcept C81820708 @default.
• W4384938557 hasConcept C86803240 @default.
• W4384938557 hasConceptScore W4384938557C100834320 @default.
• W4384938557 hasConceptScore W4384938557C100970517 @default.
• W4384938557 hasConceptScore W4384938557C104932425 @default.
• W4384938557 hasConceptScore W4384938557C114793014 @default.
• W4384938557 hasConceptScore W4384938557C126645576 @default.
• W4384938557 hasConceptScore W4384938557C127045886 @default.
• W4384938557 hasConceptScore W4384938557C127313418 @default.
• W4384938557 hasConceptScore W4384938557C136894858 @default.
• W4384938557 hasConceptScore W4384938557C187320778 @default.
• W4384938557 hasConceptScore W4384938557C18903297 @default.
• W4384938557 hasConceptScore W4384938557C193091731 @default.
• W4384938557 hasConceptScore W4384938557C197046000 @default.
• W4384938557 hasConceptScore W4384938557C197435368 @default.
• W4384938557 hasConceptScore W4384938557C205649164 @default.
• W4384938557 hasConceptScore W4384938557C49204034 @default.
• W4384938557 hasConceptScore W4384938557C50477045 @default.
• W4384938557 hasConceptScore W4384938557C58640448 @default.
• W4384938557 hasConceptScore W4384938557C76886044 @default.
• W4384938557 hasConceptScore W4384938557C81820708 @default.
• W4384938557 hasConceptScore W4384938557C86803240 @default.

• next