Matches in SemOpenAlex for { <https://semopenalex.org/work/W2316693776> ?p ?o ?g. }
- W2316693776 abstract "Abstract. The Amazon basin is a vast continental area in which atmospheric composition is relatively unaffected by anthropogenic aerosol particles. Understanding the properties of the natural biogenic aerosol particles over the Amazon rainforest is key to understanding their influence on regional and global climate. While there have been a number of studies during the wet season, and of biomass burning particles in the dry season, there has been relatively little work on the transition period – the start of the dry season in the absence of biomass burning. As part of the Brazil-UK Network for Investigation of Amazonian Atmospheric Composition and Impacts on Climate (BUNIAACIC) project, aerosol measurements, focussing on unpolluted biogenic air masses, were conducted above the canopy at a remote rainforest site in the Amazon, during the transition from wet to dry seasons, in July, 2013. This period marks the start of the dry season, but before significant biomass burning occurs in the region. Median particle number concentrations were 266 cm−3, with size distributions dominated by an accumulation mode of 130–150 nm. During periods of low particle counts, a smaller Aitken mode could also be seen around 80 nm. While the concentrations were similar in magnitude to those seen during the wet season, the size distributions suggest an enhancement in the accumulation mode compared to the wet season, but not yet to the extent seen later in the dry season, when significant biomass burning takes place. Submicron non-refractory aerosol composition, as measured by an Aerosol Chemical Speciation Monitor (ACSM), was dominated by organic material (86 %). Aerosol hygroscopicity was probed using measurements from a Hygroscopicity Tandem Differential Mobility Analyser (HTDMA), and a quasi-monodisperse Cloud Condensation Nuclei counter (CCNc). The hygroscopicity parameter, κ, was found to be low, ranging from 0.12 for Aitken mode particles to 0.18 for accumulation mode particles. This was consistent with previous studies in the region, but lower than similar measurements conducted in Borneo, where κ ranged 0.17–0.37, possibly due to a stronger marine influence at that location, bringing higher sulphate loadings than are typically seen in the Amazon. A Wide Issue Bioaerosol Sensor (WIBS-3M) was deployed at ground level to probe the coarse mode, detecting primary biological aerosol by fluorescence (Fluorescent Biological Aerosol Particles, or FBAP). The mean FBAP number concentration was 404 ± 237 l−1, however this was subject to a strong diurnal cycle, and ranged from around 200 l−1 during the day to as much as 1200 l−1 at night. FBAP dominated the coarse mode particles, comprising more than 90 % of particles detected by the WIBS-3 during the night. This proportion was also subject to a diurnal cycle, dropping to between 55 % and 75 % during the day, since non-FBAP did not show a strong diurnal pattern. Comparison with previous FBAP measurements above canopy at the same location suggests there is a strong vertical gradient in FBAP concentrations through the canopy. Application of Ward linkage cluster analysis using the z-score normalisation to the data suggests that FBAP were dominated (around 70 %) by fungal spores. Further, long-term measurements will be required in order to fully examine the seasonal variability, and distribution through the canopy of primary biological aerosol particles. This is the first time that such a suite of measurements has been deployed at this site to investigate the chemical composition and properties of the biogenic contributions to Amazonian aerosol during the transition period from the wet to dry seasons, and thus provides a unique contrast to the aerosol properties observed during the wet season in previous, similar campaigns. This was also the first deployment of a WIBS in the Amazon rainforest to study coarse mode particles, particularly primary biological aerosol particles, which is likely to play an important role as ice nuclei in the region." @default.
- W2316693776 created "2016-06-24" @default.
- W2316693776 creator A5004095631 @default.
- W2316693776 creator A5005676318 @default.
- W2316693776 creator A5009198369 @default.
- W2316693776 creator A5010983323 @default.
- W2316693776 creator A5019514358 @default.
- W2316693776 creator A5026510628 @default.
- W2316693776 creator A5047352067 @default.
- W2316693776 creator A5047704366 @default.
- W2316693776 creator A5075325330 @default.
- W2316693776 creator A5087504796 @default.
- W2316693776 creator A5089970141 @default.
- W2316693776 creator A5091507964 @default.
- W2316693776 date "2016-01-18" @default.
- W2316693776 modified "2023-09-24" @default.
- W2316693776 title "Biogenic cloud nuclei in the Amazon" @default.
- W2316693776 cites W1746440946 @default.
- W2316693776 cites W1972729264 @default.
- W2316693776 cites W1983905340 @default.
- W2316693776 cites W1993469583 @default.
- W2316693776 cites W2001372136 @default.
- W2316693776 cites W2003966715 @default.
- W2316693776 cites W2014206483 @default.
- W2316693776 cites W2018628884 @default.
- W2316693776 cites W2018637199 @default.
- W2316693776 cites W2023380448 @default.
- W2316693776 cites W2024732162 @default.
- W2316693776 cites W2026759825 @default.
- W2316693776 cites W2027833354 @default.
- W2316693776 cites W2032587168 @default.
- W2316693776 cites W2035127604 @default.
- W2316693776 cites W2036302056 @default.
- W2316693776 cites W2045504515 @default.
- W2316693776 cites W2064063882 @default.
- W2316693776 cites W2064482494 @default.
- W2316693776 cites W2069254477 @default.
- W2316693776 cites W2077475576 @default.
- W2316693776 cites W2091392780 @default.
- W2316693776 cites W2096462582 @default.
- W2316693776 cites W2098629728 @default.
- W2316693776 cites W2099636727 @default.
- W2316693776 cites W2105463749 @default.
- W2316693776 cites W2108907369 @default.
- W2316693776 cites W2117947113 @default.
- W2316693776 cites W2118306872 @default.
- W2316693776 cites W2120235685 @default.
- W2316693776 cites W2121185125 @default.
- W2316693776 cites W2121890281 @default.
- W2316693776 cites W2122315569 @default.
- W2316693776 cites W2131283510 @default.
- W2316693776 cites W2134707131 @default.
- W2316693776 cites W2137193147 @default.
- W2316693776 cites W2140779209 @default.
- W2316693776 cites W2144348006 @default.
- W2316693776 cites W2145355715 @default.
- W2316693776 cites W2149915184 @default.
- W2316693776 cites W2150859372 @default.
- W2316693776 cites W2151449194 @default.
- W2316693776 cites W2154849454 @default.
- W2316693776 cites W2155216773 @default.
- W2316693776 cites W2156377054 @default.
- W2316693776 cites W2158668210 @default.
- W2316693776 cites W2167088427 @default.
- W2316693776 cites W2167144335 @default.
- W2316693776 cites W2169002684 @default.
- W2316693776 cites W2565331444 @default.
- W2316693776 doi "https://doi.org/10.5194/acp-2015-1020" @default.
- W2316693776 hasPublicationYear "2016" @default.
- W2316693776 type Work @default.
- W2316693776 sameAs 2316693776 @default.
- W2316693776 citedByCount "1" @default.
- W2316693776 countsByYear W23166937762016 @default.
- W2316693776 crossrefType "posted-content" @default.
- W2316693776 hasAuthorship W2316693776A5004095631 @default.
- W2316693776 hasAuthorship W2316693776A5005676318 @default.
- W2316693776 hasAuthorship W2316693776A5009198369 @default.
- W2316693776 hasAuthorship W2316693776A5010983323 @default.
- W2316693776 hasAuthorship W2316693776A5019514358 @default.
- W2316693776 hasAuthorship W2316693776A5026510628 @default.
- W2316693776 hasAuthorship W2316693776A5047352067 @default.
- W2316693776 hasAuthorship W2316693776A5047704366 @default.
- W2316693776 hasAuthorship W2316693776A5075325330 @default.
- W2316693776 hasAuthorship W2316693776A5087504796 @default.
- W2316693776 hasAuthorship W2316693776A5089970141 @default.
- W2316693776 hasAuthorship W2316693776A5091507964 @default.
- W2316693776 hasBestOaLocation W23166937761 @default.
- W2316693776 hasConcept C115540264 @default.
- W2316693776 hasConcept C127313418 @default.
- W2316693776 hasConcept C153294291 @default.
- W2316693776 hasConcept C18903297 @default.
- W2316693776 hasConcept C205649164 @default.
- W2316693776 hasConcept C2619416 @default.
- W2316693776 hasConcept C2779345167 @default.
- W2316693776 hasConcept C2780001261 @default.
- W2316693776 hasConcept C39432304 @default.
- W2316693776 hasConcept C49204034 @default.
- W2316693776 hasConcept C52322663 @default.
- W2316693776 hasConcept C535291247 @default.
- W2316693776 hasConcept C86803240 @default.