FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3144320317> ?p ?o ?g. }

• W3144320317 abstract "Abstract Energy fluxes were measured by using the eddycovariance system plus an automatic weather station at thedebris-covered area on Koxkar Glacier from March toAugust, 2009. The coldest month of the glacier was Jan-uary, and air temperature reached a maximum in July andAugust. Wind velocity at 2.0 m was higher in summer andlower in winter as a whole. Precipitation was concentratedfrom May to September and accounted for about 80 % ofthe total. Daily latent heat fluxes were higher than dailysensible heat fluxes during the observation period. Themain reason for higher latent heat fluxes from March toApril was snow cover. From June to August, latent heatfluxes during the daytime were limited by surface watercontent, and were lower than sensible heat fluxes, but latentheat fluxes were higher than sensible heat fluxes duringsummer nights because of air convection in the debrislayer. Summer evaporation was higher than in the spring,and evaporation was 53.7 % of the precipitation from 19June to 23 August. The Bowen ratio ranged from -2.0 to2.0 at the site.Keywords Eddy covariance system Snow cover Precipitation Evaporation Bowen ratioIntroductionGlaciers are considered highly sensitive to climate changeand deserve attention in the context of both global changeand regional water supply (Kaser et al. 1996; Brock et al.2010). Many glacier ablation zones are mantled in near-continuous blanket of rock debris, such as the Tien Shan,Karakoram, Kunlun, Himalaya and Hengduan ranges(Zhang et al. 2011). Supraglacial debris cover on glaciersinfluences ablation regime of underlying ice by altering thesurface energy balance and imposing a barrier between theatmosphere and ice (Nicholson and Benn 2013). There is arelationship between supraglacial debris thickness and icemelt rate (Zhang et al. 2011). Very shallow layers of debrisenhance melt rates by lowering surface albedo, and thickerlayers suppress melt rates by reducing the amount of sur-face heat conducted to the ice (Reid et al. 2012; Brock et al.2010). Also, it was found that surface topography, such asslope and aspect, has an influence on total ablation (Mi-halcea et al. 2006).To project the response of glaciers to climate change, itis important to realistically describe the interactionbetween atmosphere and glacier surface (Giesen et al.2008). Several studies have been devoted to debris-coveredglaciers, to improve the understanding of the water-heatprocesses and their role in runoff from mountain regions(Mihalcea et al. 2006). Models about debris-covered gla-ciers were developed to describe how debris affects glacier" @default.
• W3144320317 created "2021-04-13" @default.
• W3144320317 creator A5036592829 @default.
• W3144320317 date "2014-01-01" @default.
• W3144320317 modified "2023-09-27" @default.
• W3144320317 title "The surface energy budget on the debris-covered Koxkar Glacier in China" @default.
• W3144320317 cites W1554656333 @default.
• W3144320317 cites W1994869682 @default.
• W3144320317 cites W2000603768 @default.
• W3144320317 cites W2007337531 @default.
• W3144320317 cites W2027722639 @default.
• W3144320317 cites W2037598088 @default.
• W3144320317 cites W2069942024 @default.
• W3144320317 cites W2070977216 @default.
• W3144320317 cites W2091933606 @default.
• W3144320317 cites W2093393225 @default.
• W3144320317 cites W2105424262 @default.
• W3144320317 cites W2110091130 @default.
• W3144320317 cites W2127831475 @default.
• W3144320317 cites W2135191259 @default.
• W3144320317 cites W2146421864 @default.
• W3144320317 cites W2152082654 @default.
• W3144320317 cites W2152973523 @default.
• W3144320317 cites W2323643732 @default.
• W3144320317 cites W2328369642 @default.
• W3144320317 cites W2378344503 @default.
• W3144320317 hasPublicationYear "2014" @default.
• W3144320317 type Work @default.
• W3144320317 sameAs 3144320317 @default.
• W3144320317 citedByCount "0" @default.
• W3144320317 crossrefType "journal-article" @default.
• W3144320317 hasAuthorship W3144320317A5036592829 @default.
• W3144320317 hasConcept C100834320 @default.
• W3144320317 hasConcept C107054158 @default.
• W3144320317 hasConcept C114793014 @default.
• W3144320317 hasConcept C127045886 @default.
• W3144320317 hasConcept C127313418 @default.
• W3144320317 hasConcept C151730666 @default.
• W3144320317 hasConcept C153294291 @default.
• W3144320317 hasConcept C197046000 @default.
• W3144320317 hasConcept C205649164 @default.
• W3144320317 hasConcept C2776023875 @default.
• W3144320317 hasConcept C2779343474 @default.
• W3144320317 hasConcept C39432304 @default.
• W3144320317 hasConcept C49204034 @default.
• W3144320317 hasConcept C58024561 @default.
• W3144320317 hasConcept C59242433 @default.
• W3144320317 hasConcept C91586092 @default.
• W3144320317 hasConceptScore W3144320317C100834320 @default.
• W3144320317 hasConceptScore W3144320317C107054158 @default.
• W3144320317 hasConceptScore W3144320317C114793014 @default.
• W3144320317 hasConceptScore W3144320317C127045886 @default.
• W3144320317 hasConceptScore W3144320317C127313418 @default.
• W3144320317 hasConceptScore W3144320317C151730666 @default.
• W3144320317 hasConceptScore W3144320317C153294291 @default.
• W3144320317 hasConceptScore W3144320317C197046000 @default.
• W3144320317 hasConceptScore W3144320317C205649164 @default.
• W3144320317 hasConceptScore W3144320317C2776023875 @default.
• W3144320317 hasConceptScore W3144320317C2779343474 @default.
• W3144320317 hasConceptScore W3144320317C39432304 @default.
• W3144320317 hasConceptScore W3144320317C49204034 @default.
• W3144320317 hasConceptScore W3144320317C58024561 @default.
• W3144320317 hasConceptScore W3144320317C59242433 @default.
• W3144320317 hasConceptScore W3144320317C91586092 @default.
• W3144320317 hasLocation W31443203171 @default.
• W3144320317 hasOpenAccess W3144320317 @default.
• W3144320317 hasPrimaryLocation W31443203171 @default.
• W3144320317 hasRelatedWork W1977089191 @default.
• W3144320317 hasRelatedWork W2018428278 @default.
• W3144320317 hasRelatedWork W2021984229 @default.
• W3144320317 hasRelatedWork W2042021062 @default.
• W3144320317 hasRelatedWork W2093879363 @default.
• W3144320317 hasRelatedWork W2162600744 @default.
• W3144320317 hasRelatedWork W2186910407 @default.
• W3144320317 hasRelatedWork W233143885 @default.
• W3144320317 hasRelatedWork W2339175387 @default.
• W3144320317 hasRelatedWork W2343676237 @default.
• W3144320317 hasRelatedWork W2372303557 @default.
• W3144320317 hasRelatedWork W2378344503 @default.
• W3144320317 hasRelatedWork W2392684098 @default.
• W3144320317 hasRelatedWork W2593447986 @default.
• W3144320317 hasRelatedWork W2752852634 @default.
• W3144320317 hasRelatedWork W2808514241 @default.
• W3144320317 hasRelatedWork W2921562839 @default.
• W3144320317 hasRelatedWork W2965222497 @default.
• W3144320317 hasRelatedWork W3093176537 @default.
• W3144320317 hasRelatedWork W53225400 @default.
• W3144320317 isParatext "false" @default.
• W3144320317 isRetracted "false" @default.
• W3144320317 magId "3144320317" @default.
• W3144320317 workType "article" @default.