2014
DOI: 10.5194/acp-14-5513-2014
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Contrasting the direct radiative effect and direct radiative forcing of aerosols

Abstract: Abstract. The direct radiative effect (DRE) of aerosols, which is the instantaneous radiative impact of all atmospheric particles on the Earth's energy balance, is sometimes confused with the direct radiative forcing (DRF), which is the change in DRE from pre-industrial to present-day (not including climate feedbacks). In this study we couple a global chemical transport model (GEOS-Chem) with a radiative transfer model (RRTMG) to contrast these concepts. We estimate a global mean all-sky aerosol DRF of −0.36 W… Show more

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Cited by 183 publications
(250 citation statements)
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References 99 publications
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“…RRTMG (Iacono et al, 2008) uses the correlated-k method to quickly calculate the atmospheric radiation flux throughout the vertical column and was implemented online into GEOSChem by Heald et al (2014), together referred to as GC-RT. RRTMG simulates extinction from water vapor, ozone, greenhouse gases, aerosols, clouds, and Rayleigh scattering over 16 longwave and 14 SW bands.…”
Section: Rrtmgmentioning
confidence: 99%
“…RRTMG (Iacono et al, 2008) uses the correlated-k method to quickly calculate the atmospheric radiation flux throughout the vertical column and was implemented online into GEOSChem by Heald et al (2014), together referred to as GC-RT. RRTMG simulates extinction from water vapor, ozone, greenhouse gases, aerosols, clouds, and Rayleigh scattering over 16 longwave and 14 SW bands.…”
Section: Rrtmgmentioning
confidence: 99%
“…In particular, assessing the radiative forcing from changes involving biogenic processes is an ongoing challenge in the modeling community but has importance in the coming decades as policymakers face decisions that depend critically on accurate knowledge of the atmospheric oxidative capacity. For example, recent studies have demonstrated the importance of considering the net effect of human-induced changes in biogenic VOC emissions on global climate forcing over the industrial period (e.g., Unger, 2014a, b;Heald et al, 2014;Heald and Spracklen, 2015). Tackling the longstanding issue of the dynamics of future global methane sources and sinks is also crucial for the next generation of climate projections (Quiquet et al, 2015;Kirschke et al, 2013).…”
Section: P Achakulwisut Et Al: Uncertainties In Isoprene Photochemimentioning
confidence: 99%
“…Recent studies have demonstrated the importance of considering the net effect of human-induced changes in biogenic VOC emissions on global climate forcing over the industrial period (e.g., Unger, 2014a, b;Heald et al, 2014;Heald and Spracklen, 2015). Unger (2014a) quantified the global radiative impact of changes to the atmospheric concentrations of ozone, methane, and SOA due to a reduction in the emission of biogenic VOCs resulting from global cropland expansion between the 1850s and 2000s.…”
Section: P Achakulwisut Et Al: Uncertainties In Isoprene Photochemimentioning
confidence: 99%
“…RRTMG (Iacono et al, 2008) uses the correlated-k method to quickly calculate the atmospheric radiation flux throughout the vertical column and was implemented online into GEOS-Chem by Heald et al (2014), together referred to as GC-RT. RRTMG simulates extinction from water vapor, ozone, greenhouse gases, aerosols, clouds and Rayleigh scattering over 16 longwave Atmos.…”
Section: Rrtmg 30mentioning
confidence: 99%