Matches in SemOpenAlex for { <https://semopenalex.org/work/W2922116286> ?p ?o ?g. }
- W2922116286 endingPage "17" @default.
- W2922116286 startingPage "1" @default.
- W2922116286 abstract "Abstract This study analyses the aerosol optical and microphysical properties obtained by the Aerosol Robotic Network (AERONET) in seven different sites operating in the Iberian Peninsula during three coincident years (2010−2012) with the objective of studying different aerosol typing approaches. This area is of interest due to its location between the Sahara desert (the largest source of natural aerosols in the world) and mainland Europe (a relevant source of anthropogenic aerosols). In particular, we study the aerosol optical depth (AOD), Angstrom parameter (α440–870) and fine mode fraction (FMF), which are estimated from direct sun irradiance measurements. Additionally, the single scattering albedo (ωo) and aerosol particle size distribution (PSD), which are computed using additional sky radiances measurements under cloudless skies, are used in our analyses. The analyses show aerosol seasonal patterns in the AOD with maximum values in summer/spring and minimum values in winter/autumn for all the analysed stations. For α440–870, there are differences from site to site, with maximum values in winter and minimum values in summer for the southern locations, while there is not a remarkable pattern for the eastern locations close to the Mediterranean coast. The frequent and intense Saharan dust outbreaks over the southern Iberian Peninsula and the intense anthropogenic activity in the eastern urban locations are behind these seasonal patterns in the AOD and α440–870. In this work, two of the most employed classification schemes of aerosol type in the literature are used: one is based on the AOD and α440–870, the other one is based on ωo at 440 nm and the FMF and a new classification scheme based on ωo at 440 nm and FMF is proposed. The results revealed that the new classification method is more appropriate for distinguishing the aerosol types that affect the Iberian Peninsula. The relationship derived here between Δωo = ωo (440)- ωo (1020) and the FMF is demonstrated to be useful for aerosol type classification when no measurements of the sky radiances, and consequently of ωo(440), are available. Alternatively, the relationship between the ratio Δωo/ωo(440) and the FMF can be used because (Δωo/ωo) provides information about both the spectral ωo and the absolute values." @default.
- W2922116286 created "2019-03-22" @default.
- W2922116286 creator A5004855874 @default.
- W2922116286 creator A5005686215 @default.
- W2922116286 creator A5013299452 @default.
- W2922116286 creator A5013568312 @default.
- W2922116286 creator A5048251952 @default.
- W2922116286 creator A5073366216 @default.
- W2922116286 creator A5085489582 @default.
- W2922116286 date "2019-08-01" @default.
- W2922116286 modified "2023-10-03" @default.
- W2922116286 title "Contribution to column-integrated aerosol typing based on Sun-photometry using different criteria" @default.
- W2922116286 cites W1500225075 @default.
- W2922116286 cites W1510008593 @default.
- W2922116286 cites W1573025181 @default.
- W2922116286 cites W1590037598 @default.
- W2922116286 cites W1602340506 @default.
- W2922116286 cites W1693050202 @default.
- W2922116286 cites W1966628118 @default.
- W2922116286 cites W1968646090 @default.
- W2922116286 cites W1973144465 @default.
- W2922116286 cites W1973744217 @default.
- W2922116286 cites W1978697436 @default.
- W2922116286 cites W1979268012 @default.
- W2922116286 cites W1981132464 @default.
- W2922116286 cites W1986973015 @default.
- W2922116286 cites W1990646419 @default.
- W2922116286 cites W1993408847 @default.
- W2922116286 cites W1993814425 @default.
- W2922116286 cites W1994870701 @default.
- W2922116286 cites W1996782635 @default.
- W2922116286 cites W1999488068 @default.
- W2922116286 cites W2003366520 @default.
- W2922116286 cites W2004020085 @default.
- W2922116286 cites W2004341293 @default.
- W2922116286 cites W2018482968 @default.
- W2922116286 cites W2020207125 @default.
- W2922116286 cites W2021934538 @default.
- W2922116286 cites W2024624865 @default.
- W2922116286 cites W2026317156 @default.
- W2922116286 cites W2035469600 @default.
- W2922116286 cites W2045258300 @default.
- W2922116286 cites W2046504998 @default.
- W2922116286 cites W2050250373 @default.
- W2922116286 cites W2050688208 @default.
- W2922116286 cites W2074513642 @default.
- W2922116286 cites W2076648945 @default.
- W2922116286 cites W2086153848 @default.
- W2922116286 cites W2089433206 @default.
- W2922116286 cites W2099997930 @default.
- W2922116286 cites W2102685893 @default.
- W2922116286 cites W2117729623 @default.
- W2922116286 cites W2120048953 @default.
- W2922116286 cites W2124321875 @default.
- W2922116286 cites W2128711297 @default.
- W2922116286 cites W2128989834 @default.
- W2922116286 cites W2133081880 @default.
- W2922116286 cites W2136408596 @default.
- W2922116286 cites W2139325971 @default.
- W2922116286 cites W2144017710 @default.
- W2922116286 cites W2152421638 @default.
- W2922116286 cites W2160214585 @default.
- W2922116286 cites W2167929905 @default.
- W2922116286 cites W2170330247 @default.
- W2922116286 cites W2502777608 @default.
- W2922116286 cites W2533091940 @default.
- W2922116286 cites W2599855932 @default.
- W2922116286 cites W2738827639 @default.
- W2922116286 cites W2757215711 @default.
- W2922116286 cites W299047321 @default.
- W2922116286 cites W4252838719 @default.
- W2922116286 cites W843664301 @default.
- W2922116286 doi "https://doi.org/10.1016/j.atmosres.2019.03.007" @default.
- W2922116286 hasPublicationYear "2019" @default.
- W2922116286 type Work @default.
- W2922116286 sameAs 2922116286 @default.
- W2922116286 citedByCount "10" @default.
- W2922116286 countsByYear W29221162862019 @default.
- W2922116286 countsByYear W29221162862020 @default.
- W2922116286 countsByYear W29221162862021 @default.
- W2922116286 countsByYear W29221162862022 @default.
- W2922116286 countsByYear W29221162862023 @default.
- W2922116286 crossrefType "journal-article" @default.
- W2922116286 hasAuthorship W2922116286A5004855874 @default.
- W2922116286 hasAuthorship W2922116286A5005686215 @default.
- W2922116286 hasAuthorship W2922116286A5013299452 @default.
- W2922116286 hasAuthorship W2922116286A5013568312 @default.
- W2922116286 hasAuthorship W2922116286A5048251952 @default.
- W2922116286 hasAuthorship W2922116286A5073366216 @default.
- W2922116286 hasAuthorship W2922116286A5085489582 @default.
- W2922116286 hasBestOaLocation W29221162862 @default.
- W2922116286 hasConcept C121332964 @default.
- W2922116286 hasConcept C126042441 @default.
- W2922116286 hasConcept C127313418 @default.
- W2922116286 hasConcept C1276947 @default.
- W2922116286 hasConcept C150846664 @default.
- W2922116286 hasConcept C153294291 @default.
- W2922116286 hasConcept C2779345167 @default.