FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2114055480> ?p ?o ?g. }

• W2114055480 endingPage "2826" @default.
• W2114055480 startingPage "2815" @default.
• W2114055480 abstract "Aerosol and surface snow samples were collected from Hidden Valley in the Dhaulagiri region of western Nepal during the summer monsoon of 1994. Temporal variations of major ion (Na+ NH4+, K+, Mg2+, Ca2+, Cl−, NO3− and SO42− concentrations in the aerosol samples are clearly related to the influx of monsoon air masses. Snow was enriched in NH4+, and NO3−, while Na+Cl− ratios were lower in the snow compared to the aerosol. A large part of this is explained by the difference in the air masses represented by aerosol and snow chemistry. Snow chemistry in general represented stronger southerly monsoon circulation, which resulted in precipitation events in Hidden Valley, whereas aerosol chemistry represented weaker monsoon or local circulation as the sampling was not conducted during rainy and foggy weather. Enrichment off NH4+ and NO3− in snow is attributed to their biogenic and agricultural sources from villages to the south and east of Hidden Valley. In addition, scavenging of HNO3 present in the air could also have contributed to the enrichment of NO3− in the snow. A lower Na+Cl−atio in snow is attributed to scavenging of HCl present locally and/or due to less fractionation of monsoon air masses during more intense circulation and shorter travel time. The observed differences in the chemistry of the two media due to the influence of monsoon versus local air masses supports the concept of using glaciochemical records from that region to interpret monsoon variations in the past. Although the aerosol samples show excess cations, our data suggest the presence of acidic gases in the air locally. The overall major soluble ion concentrations of the aerosol are comparable or lower than those measured at several other remote tropospheric sites. Our results further support the concept that high elevation mountain sites in the Himalayas can be used to investigate the composition and the evolution of the remote continental troposphere." @default.
• W2114055480 created "2016-06-24" @default.
• W2114055480 creator A5023616171 @default.
• W2114055480 creator A5043963641 @default.
• W2114055480 creator A5047977606 @default.
• W2114055480 date "1997-09-01" @default.
• W2114055480 modified "2023-10-16" @default.
• W2114055480 title "Chemical composition of aerosol and snow in the high Himalaya during the summer monsoon season" @default.
• W2114055480 cites W1482070754 @default.
• W2114055480 cites W1676703473 @default.
• W2114055480 cites W1980618234 @default.
• W2114055480 cites W1982974841 @default.
• W2114055480 cites W1987188478 @default.
• W2114055480 cites W1994941127 @default.
• W2114055480 cites W1995872439 @default.
• W2114055480 cites W2018251074 @default.
• W2114055480 cites W2021419782 @default.
• W2114055480 cites W2024891442 @default.
• W2114055480 cites W2031847508 @default.
• W2114055480 cites W2032843796 @default.
• W2114055480 cites W2034643367 @default.
• W2114055480 cites W2037553828 @default.
• W2114055480 cites W2042471852 @default.
• W2114055480 cites W2045432885 @default.
• W2114055480 cites W2063022682 @default.
• W2114055480 cites W2154397979 @default.
• W2114055480 cites W2161958842 @default.
• W2114055480 cites W2169231533 @default.
• W2114055480 cites W324969400 @default.
• W2114055480 cites W340682928 @default.
• W2114055480 cites W4251428435 @default.
• W2114055480 doi "https://doi.org/10.1016/s1352-2310(97)00047-2" @default.
• W2114055480 hasPublicationYear "1997" @default.
• W2114055480 type Work @default.
• W2114055480 sameAs 2114055480 @default.
• W2114055480 citedByCount "84" @default.
• W2114055480 countsByYear W21140554802012 @default.
• W2114055480 countsByYear W21140554802013 @default.
• W2114055480 countsByYear W21140554802014 @default.
• W2114055480 countsByYear W21140554802015 @default.
• W2114055480 countsByYear W21140554802016 @default.
• W2114055480 countsByYear W21140554802017 @default.
• W2114055480 countsByYear W21140554802018 @default.
• W2114055480 countsByYear W21140554802019 @default.
• W2114055480 countsByYear W21140554802020 @default.
• W2114055480 countsByYear W21140554802021 @default.
• W2114055480 countsByYear W21140554802022 @default.
• W2114055480 countsByYear W21140554802023 @default.
• W2114055480 crossrefType "journal-article" @default.
• W2114055480 hasAuthorship W2114055480A5023616171 @default.
• W2114055480 hasAuthorship W2114055480A5043963641 @default.
• W2114055480 hasAuthorship W2114055480A5047977606 @default.
• W2114055480 hasConcept C107054158 @default.
• W2114055480 hasConcept C107872376 @default.
• W2114055480 hasConcept C111603439 @default.
• W2114055480 hasConcept C121332964 @default.
• W2114055480 hasConcept C127313418 @default.
• W2114055480 hasConcept C136996986 @default.
• W2114055480 hasConcept C149849071 @default.
• W2114055480 hasConcept C153294291 @default.
• W2114055480 hasConcept C178790620 @default.
• W2114055480 hasConcept C185592680 @default.
• W2114055480 hasConcept C197046000 @default.
• W2114055480 hasConcept C204861789 @default.
• W2114055480 hasConcept C205649164 @default.
• W2114055480 hasConcept C2777807096 @default.
• W2114055480 hasConcept C2778004101 @default.
• W2114055480 hasConcept C2779345167 @default.
• W2114055480 hasConcept C39432304 @default.
• W2114055480 hasConcept C49204034 @default.
• W2114055480 hasConcept C55493867 @default.
• W2114055480 hasConcept C91586092 @default.
• W2114055480 hasConcept C97355855 @default.
• W2114055480 hasConceptScore W2114055480C107054158 @default.
• W2114055480 hasConceptScore W2114055480C107872376 @default.
• W2114055480 hasConceptScore W2114055480C111603439 @default.
• W2114055480 hasConceptScore W2114055480C121332964 @default.
• W2114055480 hasConceptScore W2114055480C127313418 @default.
• W2114055480 hasConceptScore W2114055480C136996986 @default.
• W2114055480 hasConceptScore W2114055480C149849071 @default.
• W2114055480 hasConceptScore W2114055480C153294291 @default.
• W2114055480 hasConceptScore W2114055480C178790620 @default.
• W2114055480 hasConceptScore W2114055480C185592680 @default.
• W2114055480 hasConceptScore W2114055480C197046000 @default.
• W2114055480 hasConceptScore W2114055480C204861789 @default.
• W2114055480 hasConceptScore W2114055480C205649164 @default.
• W2114055480 hasConceptScore W2114055480C2777807096 @default.
• W2114055480 hasConceptScore W2114055480C2778004101 @default.
• W2114055480 hasConceptScore W2114055480C2779345167 @default.
• W2114055480 hasConceptScore W2114055480C39432304 @default.
• W2114055480 hasConceptScore W2114055480C49204034 @default.
• W2114055480 hasConceptScore W2114055480C55493867 @default.
• W2114055480 hasConceptScore W2114055480C91586092 @default.
• W2114055480 hasConceptScore W2114055480C97355855 @default.
• W2114055480 hasIssue "17" @default.
• W2114055480 hasLocation W21140554801 @default.
• W2114055480 hasOpenAccess W2114055480 @default.
• W2114055480 hasPrimaryLocation W21140554801 @default.

• next