FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4281567794> ?p ?o ?g. }

• W4281567794 endingPage "867" @default.
• W4281567794 startingPage "867" @default.
• W4281567794 abstract "In the present study, we present the aerosol optical properties and radiative forcing (RF) of the tropospheric and stratospheric smoke layers, observed by the Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observation (CALIPSO) satellite, during the extraordinary Australian biomass burning (BB) event in 2019–2020. These BB layers were studied and analyzed within the longitude range 140° E–20° W and the latitude band 20°–60° S, as they were gradually transported from the Australian banks to the South American continent. These layers were found to be trapped within the Andes circulation, staying for longer time periods in the same longitude region. The BB aerosols reached altitudes even up to 22 km amsl., and regarding their optical properties, they were found to be nearly spherical (particle linear depolarization ratio (PLDR) < 0.10) in the troposphere; while, in the stratosphere, they were more depolarizing with PLDR values reaching up to 0.20. Fine and ultrafine smoke particles were dominant in the stratosphere, according to the observed Ångström exponent, related to the backscatter coefficients obtained by the pair of wavelengths 532 and 1064 nm (Åb up to 3), in contrast to the Åb values in the troposphere (Åb < 1) indicative of the presence of coarser particles. As the aerosols fend off the source, towards North America, a slightly descending trend was observed in the tropospheric Åb values, while the stratospheric ones were lightly increased. A maximum aerosol optical depth (AOD) value of 0.54 was recorded in the lower troposphere over the fire spots, while, in the stratosphere, AOD values up to 0.29 were observed. Sharp changes of carbon monoxide (CO) and ozone (O3) concentrations were also recorded by the Copernicus Atmosphere Monitoring Service (CAMS) in various atmospheric heights over the study region, associated with fire smoke emissions. The tropospheric smoke layers were found to have a negative mean radiative effect, ranging from −12.83 W/m2 at the top of the atmosphere (TOA), to −32.22 W/m2 on the surface (SRF), while the radiative effect of the stratospheric smoke was estimated between −7.36 at the TOA to −18.51 W/m2 at the SRF." @default.
• W4281567794 created "2022-05-27" @default.
• W4281567794 creator A5016796027 @default.
• W4281567794 creator A5017890165 @default.
• W4281567794 creator A5019618021 @default.
• W4281567794 creator A5042527817 @default.
• W4281567794 creator A5044293633 @default.
• W4281567794 creator A5051126831 @default.
• W4281567794 creator A5062750376 @default.
• W4281567794 creator A5067684115 @default.
• W4281567794 creator A5082748920 @default.
• W4281567794 date "2022-05-25" @default.
• W4281567794 modified "2023-10-03" @default.
• W4281567794 title "Australian Bushfires (2019–2020): Aerosol Optical Properties and Radiative Forcing" @default.
• W4281567794 cites W1499211136 @default.
• W4281567794 cites W1944755935 @default.
• W4281567794 cites W1988142639 @default.
• W4281567794 cites W1990875408 @default.
• W4281567794 cites W2003491457 @default.
• W4281567794 cites W2015471054 @default.
• W4281567794 cites W2019708954 @default.
• W4281567794 cites W2021260473 @default.
• W4281567794 cites W2050337780 @default.
• W4281567794 cites W2053692323 @default.
• W4281567794 cites W2066176117 @default.
• W4281567794 cites W2066245043 @default.
• W4281567794 cites W2097286483 @default.
• W4281567794 cites W2135419069 @default.
• W4281567794 cites W2144991971 @default.
• W4281567794 cites W2150477013 @default.
• W4281567794 cites W2151716143 @default.
• W4281567794 cites W2155129092 @default.
• W4281567794 cites W2157958981 @default.
• W4281567794 cites W2188098015 @default.
• W4281567794 cites W2295931476 @default.
• W4281567794 cites W2327754325 @default.
• W4281567794 cites W2332657826 @default.
• W4281567794 cites W2497881908 @default.
• W4281567794 cites W2511997790 @default.
• W4281567794 cites W2781682963 @default.
• W4281567794 cites W2807065520 @default.
• W4281567794 cites W2810022917 @default.
• W4281567794 cites W2885527249 @default.
• W4281567794 cites W2887212846 @default.
• W4281567794 cites W2887685367 @default.
• W4281567794 cites W2888494744 @default.
• W4281567794 cites W2900933286 @default.
• W4281567794 cites W2912696810 @default.
• W4281567794 cites W2921968109 @default.
• W4281567794 cites W2958750102 @default.
• W4281567794 cites W2961889374 @default.
• W4281567794 cites W2989833272 @default.
• W4281567794 cites W2998896996 @default.
• W4281567794 cites W3004890840 @default.
• W4281567794 cites W3030972662 @default.
• W4281567794 cites W3039970217 @default.
• W4281567794 cites W3041805507 @default.
• W4281567794 cites W3046277449 @default.
• W4281567794 cites W3088956855 @default.
• W4281567794 cites W3089076042 @default.
• W4281567794 cites W3089675041 @default.
• W4281567794 cites W3104303575 @default.
• W4281567794 cites W3110807895 @default.
• W4281567794 cites W3111576666 @default.
• W4281567794 cites W3120673662 @default.
• W4281567794 cites W3134579764 @default.
• W4281567794 cites W3134671848 @default.
• W4281567794 cites W3135753396 @default.
• W4281567794 cites W3139055800 @default.
• W4281567794 cites W3152269988 @default.
• W4281567794 cites W3169180200 @default.
• W4281567794 cites W3179857279 @default.
• W4281567794 cites W3195389616 @default.
• W4281567794 cites W3196834734 @default.
• W4281567794 cites W3215124889 @default.
• W4281567794 cites W4200235791 @default.
• W4281567794 cites W4200398753 @default.
• W4281567794 cites W4229366166 @default.
• W4281567794 doi "https://doi.org/10.3390/atmos13060867" @default.
• W4281567794 hasPublicationYear "2022" @default.
• W4281567794 type Work @default.
• W4281567794 citedByCount "2" @default.
• W4281567794 countsByYear W42815677942023 @default.
• W4281567794 crossrefType "journal-article" @default.
• W4281567794 hasAuthorship W4281567794A5016796027 @default.
• W4281567794 hasAuthorship W4281567794A5017890165 @default.
• W4281567794 hasAuthorship W4281567794A5019618021 @default.
• W4281567794 hasAuthorship W4281567794A5042527817 @default.
• W4281567794 hasAuthorship W4281567794A5044293633 @default.
• W4281567794 hasAuthorship W4281567794A5051126831 @default.
• W4281567794 hasAuthorship W4281567794A5062750376 @default.
• W4281567794 hasAuthorship W4281567794A5067684115 @default.
• W4281567794 hasAuthorship W4281567794A5082748920 @default.
• W4281567794 hasBestOaLocation W42815677941 @default.
• W4281567794 hasConcept C121332964 @default.
• W4281567794 hasConcept C122523270 @default.
• W4281567794 hasConcept C127313418 @default.
• W4281567794 hasConcept C1276947 @default.

• next