FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2593263919> ?p ?o ?g. }

• W2593263919 endingPage "56" @default.
• W2593263919 startingPage "44" @default.
• W2593263919 abstract "This paper provides an account of observed variations in Black carbon (BC) aerosol concentrations and their induced radiative forcing for the first time over Granada a measurement site in Southeastern Iberian Peninsula. Column-integrated BC concentrations were retrieved for the period 2005–2012. Monthly averages of BC concentrations (± one standard deviation) ranged from higher values in January and December with 4.0 ± 2.5 and 4 ± 3 mg/m2, respectively, to lower values in July and August with 1.6 ± 1.2 and 2.0 ± 0.5 mg/m2, respectively. This reduction is not only observed in the average values, but also in the median, third and first quartiles. The average BC concentration in winter (3.8 ± 0.6 mg/m2) was substantially higher than in summer (1.9 ± 0.3 mg/m2), being the eight-year average of 2.9 ± 0.9 mg/m2. The reduction in the use of fossil fuels during the economic crisis contributed significantly to reduced atmospheric loadings of BC. According to our analysis this situation persisted until 2010. BC concentration values were analyzed in terms of air mass influence using cluster analysis. BC concentrations for cluster 1 (local and regional areas) showed high correlations with air masses frequency in winter and autumn. In these seasons BC sources were related to the intense road traffic and increased BC emissions from domestic heating. High BC concentrations were found in autumn just when air mass frequencies for cluster 3 (Mediterranean region) were more elevated, suggesting that air masses coming from that area transport biomass burning particles towards Granada. BC aerosol optical properties were retrieved from BC fraction using aerosol AERONET size volume distribution and Mie theory. A radiative transfer model (SBDART) was used to estimate the aerosol radiative forcing separately for composite aerosol (total aerosols) and exclusively for BC aerosols. The mean radiative forcing for composite aerosol was + 23 ± 6 W/m2 (heating rate of + 0.21 ± 0.06 K/day) and + 15 ± 6 W/m2 for BC aerosol (heating rate of + 0.15 ± 0.06 K/day). These values of radiative forcing and heating rate for BC aerosol represent about 70% of their values for composite aerosol, which highlights the crucial role that BC aerosols play in modifying the radiation budget and climate." @default.
• W2593263919 created "2017-03-16" @default.
• W2593263919 creator A5007685597 @default.
• W2593263919 creator A5044723965 @default.
• W2593263919 creator A5059961959 @default.
• W2593263919 creator A5075708361 @default.
• W2593263919 creator A5085734635 @default.
• W2593263919 date "2017-07-01" @default.
• W2593263919 modified "2023-10-13" @default.
• W2593263919 title "Black carbon radiative forcing derived from AERONET measurements and models over an urban location in the southeastern Iberian Peninsula" @default.
• W2593263919 cites W1481085474 @default.
• W2593263919 cites W1560749659 @default.
• W2593263919 cites W1837497951 @default.
• W2593263919 cites W1907369419 @default.
• W2593263919 cites W1969647422 @default.
• W2593263919 cites W1981132464 @default.
• W2593263919 cites W1982689445 @default.
• W2593263919 cites W1986973015 @default.
• W2593263919 cites W1988473208 @default.
• W2593263919 cites W1989913777 @default.
• W2593263919 cites W1991240491 @default.
• W2593263919 cites W1994870701 @default.
• W2593263919 cites W1997506171 @default.
• W2593263919 cites W2010112971 @default.
• W2593263919 cites W2012610572 @default.
• W2593263919 cites W2018482968 @default.
• W2593263919 cites W2022405142 @default.
• W2593263919 cites W2026210252 @default.
• W2593263919 cites W2026317156 @default.
• W2593263919 cites W2026686956 @default.
• W2593263919 cites W2027690825 @default.
• W2593263919 cites W2028931320 @default.
• W2593263919 cites W2028999185 @default.
• W2593263919 cites W2029994529 @default.
• W2593263919 cites W2030564708 @default.
• W2593263919 cites W2031745442 @default.
• W2593263919 cites W2035875360 @default.
• W2593263919 cites W2036020873 @default.
• W2593263919 cites W2039219907 @default.
• W2593263919 cites W2045465689 @default.
• W2593263919 cites W2050250373 @default.
• W2593263919 cites W2050327836 @default.
• W2593263919 cites W2050688208 @default.
• W2593263919 cites W2065391211 @default.
• W2593263919 cites W2076158447 @default.
• W2593263919 cites W2083873585 @default.
• W2593263919 cites W2089433206 @default.
• W2593263919 cites W2102685893 @default.
• W2593263919 cites W2106721747 @default.
• W2593263919 cites W2109472798 @default.
• W2593263919 cites W2127510753 @default.
• W2593263919 cites W2139325971 @default.
• W2593263919 cites W2146034097 @default.
• W2593263919 cites W2149611009 @default.
• W2593263919 cites W2149822936 @default.
• W2593263919 cites W2150587437 @default.
• W2593263919 cites W2157507852 @default.
• W2593263919 cites W2158402318 @default.
• W2593263919 cites W2161927012 @default.
• W2593263919 cites W2163882954 @default.
• W2593263919 cites W2170982183 @default.
• W2593263919 cites W2172365426 @default.
• W2593263919 cites W2174939564 @default.
• W2593263919 cites W2179235199 @default.
• W2593263919 cites W2479952132 @default.
• W2593263919 cites W2486648408 @default.
• W2593263919 cites W2519884092 @default.
• W2593263919 cites W2519731813 @default.
• W2593263919 doi "https://doi.org/10.1016/j.atmosres.2017.03.007" @default.
• W2593263919 hasPublicationYear "2017" @default.
• W2593263919 type Work @default.
• W2593263919 sameAs 2593263919 @default.
• W2593263919 citedByCount "8" @default.
• W2593263919 countsByYear W25932639192019 @default.
• W2593263919 countsByYear W25932639192020 @default.
• W2593263919 countsByYear W25932639192021 @default.
• W2593263919 countsByYear W25932639192022 @default.
• W2593263919 countsByYear W25932639192023 @default.
• W2593263919 crossrefType "journal-article" @default.
• W2593263919 hasAuthorship W2593263919A5007685597 @default.
• W2593263919 hasAuthorship W2593263919A5044723965 @default.
• W2593263919 hasAuthorship W2593263919A5059961959 @default.
• W2593263919 hasAuthorship W2593263919A5075708361 @default.
• W2593263919 hasAuthorship W2593263919A5085734635 @default.
• W2593263919 hasBestOaLocation W25932639191 @default.
• W2593263919 hasConcept C111603439 @default.
• W2593263919 hasConcept C121332964 @default.
• W2593263919 hasConcept C123588078 @default.
• W2593263919 hasConcept C127313418 @default.
• W2593263919 hasConcept C153294291 @default.
• W2593263919 hasConcept C160529264 @default.
• W2593263919 hasConcept C166957645 @default.
• W2593263919 hasConcept C204861789 @default.
• W2593263919 hasConcept C205649164 @default.
• W2593263919 hasConcept C2776914140 @default.
• W2593263919 hasConcept C2777634575 @default.
• W2593263919 hasConcept C2779345167 @default.
• W2593263919 hasConcept C39432304 @default.

• next