FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2897584449> ?p ?o ?g. }

• W2897584449 endingPage "1513291" @default.
• W2897584449 startingPage "1513291" @default.
• W2897584449 abstract "Cloud Condensation Nuclei (CCN) concentration and aerosol size distributions in the Arctic were collected during the period 2007–2013 at the Zeppelin observatory (78.91° N, 11.89° E, 474 masl). Annual median CCN concentration at a supersaturation (SS) of 0.4% show the ranges of 45 ∼ 81 cm⁻³. The monthly median CCN number density varied between 17 cm⁻³ in October 2007 and 198 cm⁻³ in March, 2008. The CCN spectra parameters C (83 cm⁻³) and k (0.23) were derived. In addition, calculated annual median value of hygroscopicity parameter is 0.46 at SS of 0.4%. Particle number concentration of accumulation mode from aerosol size distribution measurements are well correlated with CCN concentration. The CCN to CN>10 nm (particle number concentration larger than 10nm in diameter) ratio shows a maximum during March and minimum during July. The springtime high CCN concentration is attributed to high load of accumulation mode aerosol transported from the mid-latitudes, known as Arctic Haze. CCN concentration remains high also during Arctic summer due to the source of new CCN through particle formation followed by consecutive aerosol growth. Lowest aerosol as well as CCN number densities were observed during Arctic autumn and early winter when aerosol formation in the Arctic and long-range transport into the Arctic are not effective." @default.
• W2897584449 created "2018-10-26" @default.
• W2897584449 creator A5013770173 @default.
• W2897584449 creator A5016980765 @default.
• W2897584449 creator A5017123796 @default.
• W2897584449 creator A5031427624 @default.
• W2897584449 creator A5066778274 @default.
• W2897584449 creator A5073648099 @default.
• W2897584449 creator A5081042987 @default.
• W2897584449 creator A5081228094 @default.
• W2897584449 date "2018-01-01" @default.
• W2897584449 modified "2023-10-10" @default.
• W2897584449 title "The seasonal characteristics of cloud condensation nuclei (CCN) in the arctic lower troposphere" @default.
• W2897584449 cites W1529608556 @default.
• W2897584449 cites W1921501514 @default.
• W2897584449 cites W1968654384 @default.
• W2897584449 cites W1969902735 @default.
• W2897584449 cites W1973307052 @default.
• W2897584449 cites W1981196213 @default.
• W2897584449 cites W1982838008 @default.
• W2897584449 cites W2004550998 @default.
• W2897584449 cites W2009649849 @default.
• W2897584449 cites W2012907556 @default.
• W2897584449 cites W2014741650 @default.
• W2897584449 cites W2015772592 @default.
• W2897584449 cites W2021206942 @default.
• W2897584449 cites W2031798465 @default.
• W2897584449 cites W2036351200 @default.
• W2897584449 cites W2038793415 @default.
• W2897584449 cites W2040617609 @default.
• W2897584449 cites W2040646504 @default.
• W2897584449 cites W2040984661 @default.
• W2897584449 cites W2049150358 @default.
• W2897584449 cites W2049689296 @default.
• W2897584449 cites W2062774288 @default.
• W2897584449 cites W2064943738 @default.
• W2897584449 cites W2077473119 @default.
• W2897584449 cites W2082205577 @default.
• W2897584449 cites W2086515161 @default.
• W2897584449 cites W2087035718 @default.
• W2897584449 cites W2090755408 @default.
• W2897584449 cites W2095153647 @default.
• W2897584449 cites W2095707466 @default.
• W2897584449 cites W2099636727 @default.
• W2897584449 cites W2102170561 @default.
• W2897584449 cites W2117354695 @default.
• W2897584449 cites W2119744638 @default.
• W2897584449 cites W2123405719 @default.
• W2897584449 cites W2132294853 @default.
• W2897584449 cites W2135705633 @default.
• W2897584449 cites W2136804601 @default.
• W2897584449 cites W2139472848 @default.
• W2897584449 cites W2150800280 @default.
• W2897584449 cites W2160897099 @default.
• W2897584449 cites W2164767183 @default.
• W2897584449 cites W2319467448 @default.
• W2897584449 cites W2546251245 @default.
• W2897584449 cites W2572436034 @default.
• W2897584449 cites W2583524139 @default.
• W2897584449 cites W2593629545 @default.
• W2897584449 cites W4232779659 @default.
• W2897584449 cites W4251725497 @default.
• W2897584449 doi "https://doi.org/10.1080/16000889.2018.1513291" @default.
• W2897584449 hasPublicationYear "2018" @default.
• W2897584449 type Work @default.
• W2897584449 sameAs 2897584449 @default.
• W2897584449 citedByCount "21" @default.
• W2897584449 countsByYear W28975844492020 @default.
• W2897584449 countsByYear W28975844492021 @default.
• W2897584449 countsByYear W28975844492022 @default.
• W2897584449 countsByYear W28975844492023 @default.
• W2897584449 crossrefType "journal-article" @default.
• W2897584449 hasAuthorship W2897584449A5013770173 @default.
• W2897584449 hasAuthorship W2897584449A5016980765 @default.
• W2897584449 hasAuthorship W2897584449A5017123796 @default.
• W2897584449 hasAuthorship W2897584449A5031427624 @default.
• W2897584449 hasAuthorship W2897584449A5066778274 @default.
• W2897584449 hasAuthorship W2897584449A5073648099 @default.
• W2897584449 hasAuthorship W2897584449A5081042987 @default.
• W2897584449 hasAuthorship W2897584449A5081228094 @default.
• W2897584449 hasBestOaLocation W28975844491 @default.
• W2897584449 hasConcept C111368507 @default.
• W2897584449 hasConcept C121332964 @default.
• W2897584449 hasConcept C127313418 @default.
• W2897584449 hasConcept C153294291 @default.
• W2897584449 hasConcept C178790620 @default.
• W2897584449 hasConcept C185592680 @default.
• W2897584449 hasConcept C200447597 @default.
• W2897584449 hasConcept C2779345167 @default.
• W2897584449 hasConcept C33332676 @default.
• W2897584449 hasConcept C39432304 @default.
• W2897584449 hasConcept C518008717 @default.
• W2897584449 hasConcept C79974267 @default.
• W2897584449 hasConcept C9075549 @default.
• W2897584449 hasConcept C91586092 @default.
• W2897584449 hasConceptScore W2897584449C111368507 @default.
• W2897584449 hasConceptScore W2897584449C121332964 @default.
• W2897584449 hasConceptScore W2897584449C127313418 @default.

• next