FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2899580056> ?p ?o ?g. }

• W2899580056 endingPage "2217" @default.
• W2899580056 startingPage "2201" @default.
• W2899580056 abstract "Abstract. Aerosol extinction coefficients (σa) and lidar ratios (LRs) are retrieved over the ocean from CALIPSO's Cloud-Aerosol Lidar with Orthogonal Polarization (CALIOP) attenuated backscatter profiles by solving the lidar equation constrained with aerosol optical depths (AODs) derived by applying the Synergized Optical Depth of Aerosols (SODA) algorithm to ocean surface returns measured by CALIOP and CloudSat's Cloud Profiling Radar. σa and LR are retrieved for two independent scenarios that require somewhat different assumptions: (a) a single homogeneous atmospheric layer (1L) for which the LR is constant with height and (b) a vertically homogeneous layer with a constant LR overlying a marine boundary layer with a homogenous LR fixed at 25 sr (two-layer method, 2L). These new retrievals differ from the standard CALIPSO version 4.1 (V4) product, as the CALIOP–SODA method does not rely on an aerosol classification scheme to select LR. CALIOP–SODA σa and LR are evaluated using airborne high-spectral-resolution lidar (HSRL) observations over the northwest Atlantic. CALIOP–SODA LR (1L and 2L) positively correlates with its HSRL counterpart (linear correlation coefficient r>0.67), with a negative bias smaller than 17.4 % and a good agreement for σa (r≥0.78) with a small negative bias (≤|-9.2%|). Furthermore, a global comparison of optical depths derived by CALIOP–SODA and CALIPSO V4 reveals substantial discrepancies over regions dominated by dust and smoke (0.24), whereas Aqua's Moderate resolution Imaging Spectroradiometer (MODIS) and SODA AOD regional differences are within 0.06. Global maps of CALIOP–SODA LR feature high values over littoral zones, consistent with expectations of continental aerosol transport offshore. In addition, seasonal transitions associated with biomass burning from June to October over the southeast Atlantic are well reproduced by CALIOP–SODA LR." @default.
• W2899580056 created "2018-11-16" @default.
• W2899580056 creator A5011062870 @default.
• W2899580056 creator A5015916153 @default.
• W2899580056 creator A5050221285 @default.
• W2899580056 creator A5056870102 @default.
• W2899580056 creator A5086822111 @default.
• W2899580056 creator A5087669885 @default.
• W2899580056 date "2019-04-10" @default.
• W2899580056 modified "2023-10-16" @default.
• W2899580056 title "Novel aerosol extinction coefficients and lidar ratios over the ocean from CALIPSO–CloudSat: evaluation and global statistics" @default.
• W2899580056 cites W1828003706 @default.
• W2899580056 cites W1850578838 @default.
• W2899580056 cites W1917501116 @default.
• W2899580056 cites W1978128070 @default.
• W2899580056 cites W1978732256 @default.
• W2899580056 cites W1982755993 @default.
• W2899580056 cites W1982916037 @default.
• W2899580056 cites W1983545043 @default.
• W2899580056 cites W1989426046 @default.
• W2899580056 cites W2002311377 @default.
• W2899580056 cites W2003491457 @default.
• W2899580056 cites W2010407021 @default.
• W2899580056 cites W2012546069 @default.
• W2899580056 cites W2014106555 @default.
• W2899580056 cites W2015471054 @default.
• W2899580056 cites W2021260473 @default.
• W2899580056 cites W2023268507 @default.
• W2899580056 cites W2026231838 @default.
• W2899580056 cites W2028425992 @default.
• W2899580056 cites W2031090686 @default.
• W2899580056 cites W2043267560 @default.
• W2899580056 cites W2046297721 @default.
• W2899580056 cites W2048078755 @default.
• W2899580056 cites W2053692323 @default.
• W2899580056 cites W2058252484 @default.
• W2899580056 cites W2071732967 @default.
• W2899580056 cites W2073348927 @default.
• W2899580056 cites W2073904902 @default.
• W2899580056 cites W2084854086 @default.
• W2899580056 cites W2087199341 @default.
• W2899580056 cites W2087818999 @default.
• W2899580056 cites W2089178461 @default.
• W2899580056 cites W2090693450 @default.
• W2899580056 cites W2093215882 @default.
• W2899580056 cites W2095967171 @default.
• W2899580056 cites W2098209866 @default.
• W2899580056 cites W2103397097 @default.
• W2899580056 cites W2103977502 @default.
• W2899580056 cites W2104900072 @default.
• W2899580056 cites W2108688260 @default.
• W2899580056 cites W2108985441 @default.
• W2899580056 cites W2111934362 @default.
• W2899580056 cites W2114865141 @default.
• W2899580056 cites W2118175980 @default.
• W2899580056 cites W2121570253 @default.
• W2899580056 cites W2124552978 @default.
• W2899580056 cites W2130672574 @default.
• W2899580056 cites W2132902101 @default.
• W2899580056 cites W2137121736 @default.
• W2899580056 cites W2143089171 @default.
• W2899580056 cites W2143580731 @default.
• W2899580056 cites W2144991971 @default.
• W2899580056 cites W2156645902 @default.
• W2899580056 cites W2400393067 @default.
• W2899580056 cites W2407627142 @default.
• W2899580056 cites W2567120496 @default.
• W2899580056 cites W2597124476 @default.
• W2899580056 cites W2618665912 @default.
• W2899580056 cites W2689816714 @default.
• W2899580056 cites W2749220154 @default.
• W2899580056 cites W2755859357 @default.
• W2899580056 cites W2769431611 @default.
• W2899580056 cites W2786092450 @default.
• W2899580056 cites W2788932994 @default.
• W2899580056 cites W2810022917 @default.
• W2899580056 cites W2843634981 @default.
• W2899580056 cites W2884761458 @default.
• W2899580056 cites W2892842538 @default.
• W2899580056 doi "https://doi.org/10.5194/amt-12-2201-2019" @default.
• W2899580056 hasPublicationYear "2019" @default.
• W2899580056 type Work @default.
• W2899580056 sameAs 2899580056 @default.
• W2899580056 citedByCount "12" @default.
• W2899580056 countsByYear W28995800562020 @default.
• W2899580056 countsByYear W28995800562021 @default.
• W2899580056 countsByYear W28995800562022 @default.
• W2899580056 countsByYear W28995800562023 @default.
• W2899580056 crossrefType "journal-article" @default.
• W2899580056 hasAuthorship W2899580056A5011062870 @default.
• W2899580056 hasAuthorship W2899580056A5015916153 @default.
• W2899580056 hasAuthorship W2899580056A5050221285 @default.
• W2899580056 hasAuthorship W2899580056A5056870102 @default.
• W2899580056 hasAuthorship W2899580056A5086822111 @default.
• W2899580056 hasAuthorship W2899580056A5087669885 @default.
• W2899580056 hasBestOaLocation W28995800561 @default.
• W2899580056 hasConcept C101991246 @default.
• W2899580056 hasConcept C121332964 @default.

• next