Estimates of global multicomponent aerosol optical depth and direct radiative perturbation in the Laboratoire de Météorologie Dynamique general circulation model

By M. Reddy, O. Boucher, N. Bellouin, Michael Schulz, Y. Balkanski, J. Dufresne, M. Pham. 2005

164 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/edaa1770caee5f434d8571a57b57bc46d89117da

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In Atmospheric Science

In Global and Planetary Change

Citations in the corpus

SALSA – a Sectional Aerosol module for Large Scale Applications (2007, background): “Another way of tackling this problem is to apply the sectional approach for some of the aerosol sizes and to treat the rest of the aerosol sizes using either modal or bulk mass based approach (Liao and Seinfeld, 2005; Liu et al., 2005; Reddy et al., 2005).”
Investigating cloud absorption effects: Global absorption properties of black carbon, tar balls, and soil dust in clouds and aerosols (2012, result): “…the model compared with data contrasts with some earlier studies that found model underpredictions of AAOD with AERONET data in particular [Sato et al., 2003; Reddy et al., 2005], most likely due to the treatment of BC as externally mixed as opposed to evolving between external and internal mixing.”
Analysis and quantification of the diversities of aerosol life cycles within AeroCom (2005, unknown): “…Tiedtke (1989), contributes to total condensed water but not to cloud fraction Boucher et al. (2002); Reddy et al. (2005) Boucher et al. (2002); Reddy et al. (2005) as liquid (in cloud-scav only) all: 0.3 MATCH Rasch and Kristjansson (1998) Zhang and McFarlane (1995b) Rasch et al. (2000) Rasch…”
Simulation of direct radiative forcing of aerosols and their effects on East Asian climate using an interactive AGCM-aerosol coupled system (2012, methodology): “The Laboratoire de Météorologie Dynamique GCM coupled with a multi-component aerosol module was used to estimate the global annual average DRF and got a value of -1.04 W m-2 at the TOA due to total aerosols in all-sky condition (Reddy et al. 2005).”