FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2177388210> ?p ?o ?g. }

• W2177388210 endingPage "12933" @default.
• W2177388210 startingPage "12909" @default.
• W2177388210 abstract "Abstract. Aerosols affect the atmosphere through direct interaction with short-wave and long-wave radiation and the microphysical properties of clouds. In this paper we report in detail on several mechanisms by which the short-term impact of dust on surface radiative fluxes can affect the dust loading of the atmosphere via modification of boundary-layer meteorology. This in turn affects the aerosol radiative forcing itself. Examples of these feedbacks between dust and boundary layer meteorology were observed during a series of dust storms in the Sahara and the eastern Mediterranean in April 2012. These case studies have been analysed using the Monitoring Atmospheric Composition and Climate – Interim Implementation (MACC-II) system. The radiative fluxes in the short-wave and long-wave spectra were both significantly affected by the prognostic aerosol–radiation interaction, which in turn impacted the meteorological simulation. Reduced incoming solar radiation below the aerosol layers led to a decrease in maximum surface temperatures and to a more stable thermal stratification of the lower atmosphere. This in turn forced weaker surface wind speeds and eventually smaller dust emissions. Moreover, we also observed a secondary impact of the aerosol radiative forcing, whereby horizontal gradients of surface temperature were increased at the edge of the dust plume, which led to local increases of surface wind speeds due to the thermal wind effect. The differentiated impact of the aerosol layer on surface pressure also contributed to the increase in surface wind speed and dust production in the same area. Enhanced long-wave radiative fluxes by the dust mass were associated with opposite processes. Less stable thermal stratification at night, brought mainly by higher minimum temperatures at the surface, caused stronger surface winds. At the edge of the dust storm, weaker horizontal temperature and pressure gradients forced lower winds and reduced dust production. Regarding dust emissions, short-wave radiative forcing had a larger impact than long-wave radiative forcing, corroborating several previous studies. For surface temperature, short-wave and long-wave contribution were close in intensity. These feedbacks were amplified when using data assimilation to build the aerosol analysis of the MACC-II global system. This led to an improvement in the short-term forecasts of thermal radiative fluxes and surface temperatures." @default.
• W2177388210 created "2016-06-24" @default.
• W2177388210 creator A5019775443 @default.
• W2177388210 creator A5038866291 @default.
• W2177388210 creator A5042031409 @default.
• W2177388210 creator A5050506862 @default.
• W2177388210 creator A5053550200 @default.
• W2177388210 creator A5062518836 @default.
• W2177388210 creator A5067207325 @default.
• W2177388210 creator A5073096063 @default.
• W2177388210 creator A5076646154 @default.
• W2177388210 creator A5088856954 @default.
• W2177388210 date "2015-11-20" @default.
• W2177388210 modified "2023-09-26" @default.
• W2177388210 title "Feedbacks of dust and boundary layer meteorology during a dust storm in the eastern Mediterranean" @default.
• W2177388210 cites W118893451 @default.
• W2177388210 cites W1964549182 @default.
• W2177388210 cites W1967385161 @default.
• W2177388210 cites W1970047006 @default.
• W2177388210 cites W1973755324 @default.
• W2177388210 cites W1979651770 @default.
• W2177388210 cites W1980051980 @default.
• W2177388210 cites W1987461785 @default.
• W2177388210 cites W1990213571 @default.
• W2177388210 cites W1993065427 @default.
• W2177388210 cites W1998647656 @default.
• W2177388210 cites W2003362896 @default.
• W2177388210 cites W2008874157 @default.
• W2177388210 cites W2009849014 @default.
• W2177388210 cites W2013703069 @default.
• W2177388210 cites W2020075529 @default.
• W2177388210 cites W2021606238 @default.
• W2177388210 cites W2034445943 @default.
• W2177388210 cites W2039874658 @default.
• W2177388210 cites W2065839317 @default.
• W2177388210 cites W2068106641 @default.
• W2177388210 cites W2069261600 @default.
• W2177388210 cites W2069270217 @default.
• W2177388210 cites W2076783983 @default.
• W2177388210 cites W2078517784 @default.
• W2177388210 cites W2081928990 @default.
• W2177388210 cites W2083340840 @default.
• W2177388210 cites W2083471549 @default.
• W2177388210 cites W2087240094 @default.
• W2177388210 cites W2088848786 @default.
• W2177388210 cites W2089143267 @default.
• W2177388210 cites W2089433206 @default.
• W2177388210 cites W2092548950 @default.
• W2177388210 cites W2093674996 @default.
• W2177388210 cites W2094408786 @default.
• W2177388210 cites W2096228125 @default.
• W2177388210 cites W2100657879 @default.
• W2177388210 cites W2102134204 @default.
• W2177388210 cites W2111033742 @default.
• W2177388210 cites W2111212225 @default.
• W2177388210 cites W2126167934 @default.
• W2177388210 cites W2128791277 @default.
• W2177388210 cites W2130578813 @default.
• W2177388210 cites W2136481087 @default.
• W2177388210 cites W2137121736 @default.
• W2177388210 cites W2143063774 @default.
• W2177388210 cites W2153438006 @default.
• W2177388210 cites W2156096080 @default.
• W2177388210 cites W2161987407 @default.
• W2177388210 cites W2166055221 @default.
• W2177388210 cites W2166786685 @default.
• W2177388210 cites W2177292717 @default.
• W2177388210 doi "https://doi.org/10.5194/acp-15-12909-2015" @default.
• W2177388210 hasPublicationYear "2015" @default.
• W2177388210 type Work @default.
• W2177388210 sameAs 2177388210 @default.
• W2177388210 citedByCount "36" @default.
• W2177388210 countsByYear W21773882102016 @default.
• W2177388210 countsByYear W21773882102017 @default.
• W2177388210 countsByYear W21773882102018 @default.
• W2177388210 countsByYear W21773882102019 @default.
• W2177388210 countsByYear W21773882102020 @default.
• W2177388210 countsByYear W21773882102021 @default.
• W2177388210 countsByYear W21773882102022 @default.
• W2177388210 countsByYear W21773882102023 @default.
• W2177388210 crossrefType "journal-article" @default.
• W2177388210 hasAuthorship W2177388210A5019775443 @default.
• W2177388210 hasAuthorship W2177388210A5038866291 @default.
• W2177388210 hasAuthorship W2177388210A5042031409 @default.
• W2177388210 hasAuthorship W2177388210A5050506862 @default.
• W2177388210 hasAuthorship W2177388210A5053550200 @default.
• W2177388210 hasAuthorship W2177388210A5062518836 @default.
• W2177388210 hasAuthorship W2177388210A5067207325 @default.
• W2177388210 hasAuthorship W2177388210A5073096063 @default.
• W2177388210 hasAuthorship W2177388210A5076646154 @default.
• W2177388210 hasAuthorship W2177388210A5088856954 @default.
• W2177388210 hasBestOaLocation W21773882101 @default.
• W2177388210 hasConcept C105306849 @default.
• W2177388210 hasConcept C111603439 @default.
• W2177388210 hasConcept C121332964 @default.
• W2177388210 hasConcept C127313418 @default.
• W2177388210 hasConcept C153294291 @default.
• W2177388210 hasConcept C153385146 @default.

• next