Matches in SemOpenAlex for { <https://semopenalex.org/work/W2017783890> ?p ?o ?g. }
- W2017783890 endingPage "10690" @default.
- W2017783890 startingPage "10679" @default.
- W2017783890 abstract "Abstract. The present paper investigates the diurnal and seasonal variability of the aerosol total number concentration, number and volume size distribution between 10 nm and 10 μm, from a combination of a scanning mobility particle sizer (SMPS) and an optical counter (OPC), performed over a two-year period (January 2006–February 2008) at the Nepal Climate Observatory-Pyramid (NCO-P) research station, (5079 m a.s.l.). The annual average number concentration measured over the two-year period at the NCO-P is 860 cm−3. Total concentrations show a strong seasonality with maxima during pre-monsoon and post-monsoon seasons and minima during the dry and monsoon seasons. A diurnal variation is also clearly observed, with maxima between 09:00 and 12:00 UTC. The aerosol concentration maxima are mainly due to nucleation processes during the post-monsoon season, as witnessed by high nucleation mode integrated number concentrations, and to transport of high levels of pollution from the plains by valley breezes during the pre-monsoon season, as demonstrated by high accumulation mode integrated number concentrations. Night-time number concentration of particles (from 03:00 to 08:00 NST) are relatively low throughout the year (from 450 cm−3 during the monsoon season to 675 cm−3 during the pre-monsoon season), indicating the of high altitudes background level, as a result of downslope winds during this part of the day. However, it was found that these background concentrations are strongly influenced by the daytime concentrations, as they show the same seasonal variability. If nighttime concentrations were presumed to be representative of free troposphere (FT)/residual layer concentrations, they would be found to be two times higher than at other lower altitudes European sites, such as the Jungfraujoch. However, BL intrusions might contaminate the free troposphere/residual layer even at this altitude, especially during regional air masses influence. Night-time measurements were subsequently selected to study the FT composition according to different air masses, and the effect of long range transport to the station." @default.
- W2017783890 created "2016-06-24" @default.
- W2017783890 creator A5005650821 @default.
- W2017783890 creator A5013159030 @default.
- W2017783890 creator A5031423755 @default.
- W2017783890 creator A5033428767 @default.
- W2017783890 creator A5061772292 @default.
- W2017783890 creator A5062255096 @default.
- W2017783890 creator A5064076320 @default.
- W2017783890 creator A5067769357 @default.
- W2017783890 creator A5076904933 @default.
- W2017783890 creator A5084521253 @default.
- W2017783890 date "2010-11-12" @default.
- W2017783890 modified "2023-09-30" @default.
- W2017783890 title "Seasonal variations of aerosol size distributions based on long-term measurements at the high altitude Himalayan site of Nepal Climate Observatory-Pyramid (5079 m), Nepal" @default.
- W2017783890 cites W1988473208 @default.
- W2017783890 cites W1993603582 @default.
- W2017783890 cites W1993769151 @default.
- W2017783890 cites W2000762356 @default.
- W2017783890 cites W2021984751 @default.
- W2017783890 cites W2023077614 @default.
- W2017783890 cites W2028826232 @default.
- W2017783890 cites W2033905335 @default.
- W2017783890 cites W2036025639 @default.
- W2017783890 cites W2061836473 @default.
- W2017783890 cites W2068842930 @default.
- W2017783890 cites W2089084307 @default.
- W2017783890 cites W2093739432 @default.
- W2017783890 cites W2093861976 @default.
- W2017783890 cites W2098651037 @default.
- W2017783890 cites W2099906647 @default.
- W2017783890 cites W2108288504 @default.
- W2017783890 cites W2115251260 @default.
- W2017783890 cites W2116817581 @default.
- W2017783890 cites W2118677261 @default.
- W2017783890 cites W2119744638 @default.
- W2017783890 cites W2121133053 @default.
- W2017783890 cites W2124061257 @default.
- W2017783890 cites W2126696183 @default.
- W2017783890 cites W2131041319 @default.
- W2017783890 cites W2132843990 @default.
- W2017783890 cites W2134199848 @default.
- W2017783890 cites W2137739275 @default.
- W2017783890 cites W2140334361 @default.
- W2017783890 cites W2151873733 @default.
- W2017783890 cites W2154836345 @default.
- W2017783890 cites W2161621332 @default.
- W2017783890 cites W2170571179 @default.
- W2017783890 cites W2171180612 @default.
- W2017783890 cites W4211242048 @default.
- W2017783890 doi "https://doi.org/10.5194/acp-10-10679-2010" @default.
- W2017783890 hasPublicationYear "2010" @default.
- W2017783890 type Work @default.
- W2017783890 sameAs 2017783890 @default.
- W2017783890 citedByCount "40" @default.
- W2017783890 countsByYear W20177838902012 @default.
- W2017783890 countsByYear W20177838902013 @default.
- W2017783890 countsByYear W20177838902014 @default.
- W2017783890 countsByYear W20177838902015 @default.
- W2017783890 countsByYear W20177838902016 @default.
- W2017783890 countsByYear W20177838902017 @default.
- W2017783890 countsByYear W20177838902018 @default.
- W2017783890 countsByYear W20177838902019 @default.
- W2017783890 countsByYear W20177838902020 @default.
- W2017783890 countsByYear W20177838902021 @default.
- W2017783890 countsByYear W20177838902022 @default.
- W2017783890 crossrefType "journal-article" @default.
- W2017783890 hasAuthorship W2017783890A5005650821 @default.
- W2017783890 hasAuthorship W2017783890A5013159030 @default.
- W2017783890 hasAuthorship W2017783890A5031423755 @default.
- W2017783890 hasAuthorship W2017783890A5033428767 @default.
- W2017783890 hasAuthorship W2017783890A5061772292 @default.
- W2017783890 hasAuthorship W2017783890A5062255096 @default.
- W2017783890 hasAuthorship W2017783890A5064076320 @default.
- W2017783890 hasAuthorship W2017783890A5067769357 @default.
- W2017783890 hasAuthorship W2017783890A5076904933 @default.
- W2017783890 hasAuthorship W2017783890A5084521253 @default.
- W2017783890 hasBestOaLocation W20177838901 @default.
- W2017783890 hasConcept C125403950 @default.
- W2017783890 hasConcept C127313418 @default.
- W2017783890 hasConcept C136996986 @default.
- W2017783890 hasConcept C142362112 @default.
- W2017783890 hasConcept C153294291 @default.
- W2017783890 hasConcept C162725370 @default.
- W2017783890 hasConcept C167678106 @default.
- W2017783890 hasConcept C18903297 @default.
- W2017783890 hasConcept C205649164 @default.
- W2017783890 hasConcept C2524010 @default.
- W2017783890 hasConcept C2779345167 @default.
- W2017783890 hasConcept C33923547 @default.
- W2017783890 hasConcept C39432304 @default.
- W2017783890 hasConcept C49204034 @default.
- W2017783890 hasConcept C52119013 @default.
- W2017783890 hasConcept C554144382 @default.
- W2017783890 hasConcept C6350597 @default.
- W2017783890 hasConcept C86803240 @default.
- W2017783890 hasConcept C91528185 @default.
- W2017783890 hasConcept C91586092 @default.