FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W46509103> ?p ?o ?g. }

• W46509103 abstract "Tropospheric aerosols, from natural and anthropogenic sources, may have a significant influence on the radiative balance of the Earth by their direct and indirect effects. The a im of this paper is to study the interactions between aerosol particles (SO4 2- ) and the cloud radiative properties. Consequently, using the production p arameters and bu rdens of SO4 2- predicted b y eleven chemical t ransport models, we have calculated the microphysical parameters: liquid water content, cloud d roplet number concentration, effective radius, cloud albedo, and the susceptibility (the sensitivity of cloud albedo to changes in cloud droplet number concentration(CDNC)). The relationships proposed by Boucher and Lohmann (1995) and by Menon and Saxena (1998) were used to compare the values of CDNC for maritime and continental clouds. The obtained values of the cloud p arameters with these relationships are in agreement with the results from satellitare data for small amounts of sulfate mass concentration. Consequently, new approximations or corrections are necessary for the relationships between aerosol sulfate mass and cloud droplet number concentrations, for higher values of sulfate amount. Aerosols have a direct radiative forcing because they scatter and absorb solar and infrared radiation in the atmosphere. Aerosols also alter the formation and precipitation efficiency of liquid-water, ice and mixed-phase clouds, thereby causing an indirect radiative forcing associated with the changes in cloud properties. The quantification o f aerosol radiative forcing is more complex than the quantification o f greenhouse gases radiative forcing because aerosol mass and particle number concentrations are highly v ariable in space and time. The indirect effects (Twomey, 1977, Albrecht, 1989, and Pincus and Baker, 1994) are far more complex and more difficult to assess than the direct effect, because they depend on a chain o f phenomena that connect chemical and physical properties of aerosol to concentration o f cloud condensation n uclei (CCN), then CCN concentrations to cloud droplet number concentrations (CDNC) and these, in turn, the cloud albedo. Therefore, it is a great challenge in adequately characterising the nature and occurrence of atmospheric aerosols and in including their effects in models to reduce uncertainties in climate prediction. Large uncertainties appears because aerosols: originate from a variety o f sources, are distributed across a wide spectrum of" @default.
• W46509103 created "2016-06-24" @default.
• W46509103 creator A5023205954 @default.
• W46509103 creator A5030334124 @default.
• W46509103 creator A5070209266 @default.
• W46509103 date "2003-01-01" @default.
• W46509103 modified "2023-10-18" @default.
• W46509103 title "INFLUENCE OF SULFATE AEROSOL PARTICLES ON RADIATIVE PROPERTIES OF CLOUDS" @default.
• W46509103 cites W1969553711 @default.
• W46509103 cites W1982254235 @default.
• W46509103 cites W1986006395 @default.
• W46509103 cites W1993717104 @default.
• W46509103 cites W1994699491 @default.
• W46509103 cites W1996959164 @default.
• W46509103 cites W2004174878 @default.
• W46509103 cites W2009239784 @default.
• W46509103 cites W2012910700 @default.
• W46509103 cites W2014196541 @default.
• W46509103 cites W2019906359 @default.
• W46509103 cites W2023222351 @default.
• W46509103 cites W2037568311 @default.
• W46509103 cites W2042112467 @default.
• W46509103 cites W2053583276 @default.
• W46509103 cites W2059584473 @default.
• W46509103 cites W2069461995 @default.
• W46509103 cites W2070804679 @default.
• W46509103 cites W2071531062 @default.
• W46509103 cites W2071800039 @default.
• W46509103 cites W2075609411 @default.
• W46509103 cites W2095245634 @default.
• W46509103 cites W2097160124 @default.
• W46509103 cites W2138435984 @default.
• W46509103 cites W2143024498 @default.
• W46509103 cites W2150966988 @default.
• W46509103 cites W2173852084 @default.
• W46509103 cites W297421864 @default.
• W46509103 hasPublicationYear "2003" @default.
• W46509103 type Work @default.
• W46509103 sameAs 46509103 @default.
• W46509103 citedByCount "0" @default.
• W46509103 crossrefType "journal-article" @default.
• W46509103 hasAuthorship W46509103A5023205954 @default.
• W46509103 hasAuthorship W46509103A5030334124 @default.
• W46509103 hasAuthorship W46509103A5070209266 @default.
• W46509103 hasConcept C111919701 @default.
• W46509103 hasConcept C114203453 @default.
• W46509103 hasConcept C121332964 @default.
• W46509103 hasConcept C142362112 @default.
• W46509103 hasConcept C153294291 @default.
• W46509103 hasConcept C153385146 @default.
• W46509103 hasConcept C169969230 @default.
• W46509103 hasConcept C178790620 @default.
• W46509103 hasConcept C185592680 @default.
• W46509103 hasConcept C195886398 @default.
• W46509103 hasConcept C206887242 @default.
• W46509103 hasConcept C2778343803 @default.
• W46509103 hasConcept C2778804858 @default.
• W46509103 hasConcept C2779345167 @default.
• W46509103 hasConcept C2779406902 @default.
• W46509103 hasConcept C39432304 @default.
• W46509103 hasConcept C41008148 @default.
• W46509103 hasConcept C52119013 @default.
• W46509103 hasConcept C554144382 @default.
• W46509103 hasConcept C62520636 @default.
• W46509103 hasConcept C7337166 @default.
• W46509103 hasConcept C74902906 @default.
• W46509103 hasConcept C75115192 @default.
• W46509103 hasConcept C79974875 @default.
• W46509103 hasConcept C85502700 @default.
• W46509103 hasConcept C91586092 @default.
• W46509103 hasConcept C98444146 @default.
• W46509103 hasConcept C99578197 @default.
• W46509103 hasConceptScore W46509103C111919701 @default.
• W46509103 hasConceptScore W46509103C114203453 @default.
• W46509103 hasConceptScore W46509103C121332964 @default.
• W46509103 hasConceptScore W46509103C142362112 @default.
• W46509103 hasConceptScore W46509103C153294291 @default.
• W46509103 hasConceptScore W46509103C153385146 @default.
• W46509103 hasConceptScore W46509103C169969230 @default.
• W46509103 hasConceptScore W46509103C178790620 @default.
• W46509103 hasConceptScore W46509103C185592680 @default.
• W46509103 hasConceptScore W46509103C195886398 @default.
• W46509103 hasConceptScore W46509103C206887242 @default.
• W46509103 hasConceptScore W46509103C2778343803 @default.
• W46509103 hasConceptScore W46509103C2778804858 @default.
• W46509103 hasConceptScore W46509103C2779345167 @default.
• W46509103 hasConceptScore W46509103C2779406902 @default.
• W46509103 hasConceptScore W46509103C39432304 @default.
• W46509103 hasConceptScore W46509103C41008148 @default.
• W46509103 hasConceptScore W46509103C52119013 @default.
• W46509103 hasConceptScore W46509103C554144382 @default.
• W46509103 hasConceptScore W46509103C62520636 @default.
• W46509103 hasConceptScore W46509103C7337166 @default.
• W46509103 hasConceptScore W46509103C74902906 @default.
• W46509103 hasConceptScore W46509103C75115192 @default.
• W46509103 hasConceptScore W46509103C79974875 @default.
• W46509103 hasConceptScore W46509103C85502700 @default.
• W46509103 hasConceptScore W46509103C91586092 @default.
• W46509103 hasConceptScore W46509103C98444146 @default.
• W46509103 hasConceptScore W46509103C99578197 @default.

• next