Single-Scattering Albedo and Radiative Forcing of Various Aerosol Species with a Global Three-Dimensional Model

By Toshihiko Takemura, Teruyuki Nakajima, Oleg Dubovik, Brent N. Holben, S. Kinne. 2002

505 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/5c7663e08c3776048a20e07d0fdc144bb41f0716

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Citations in the corpus

Estimates of global multicomponent aerosol optical depth and direct radiative perturbation in the Laboratoire de Météorologie Dynamique general circulation model (2005, methodology): “addressing different facets of aerosol-climate interactions [Liao et al., 2004; Jacobson, 2001; Takemura et al., 2002; Chin et al., 2002; Chuang et al., 2002].”
Analysis and quantification of the diversities of aerosol life cycles within AeroCom (2005, unknown): “…et al. (2001) bin, modal M for aerosol dyn ** 17 bins 10 DU, 4 SS, 1 BC, 1 BCPOM, 1 SO4 (5 modes for aerosol dyn) ext partly int for BC/ POM none Takemura et al. (2000, 2002, 2005) ); Guelle et al. (1998a, b, 2000); Smith and Harrison (1998); Balkanski et al. (2003); Bauer et al. (2004); Schulz…”
Whitecap coverage from satellite measurements: A first step toward modeling the variability of oceanic whitecaps (2006, background): “…the potential to mitigate global warming directly by increasing planetary albedo [Haywood et al., 1999; Winter and Chýlek, 1997; Jacobson, 2001; Takemura et al., 2002; Grini et al., 2002; Liao et al., 2004], indirectly by acting as cloud condensation nuclei (CCN) thus altering cloud albedo…”
Influences of in-cloud aerosol scavenging parameterizations on aerosol concentrations and wet deposition in ECHAM5-HAM (2009, methodology): “Prescribed aerosol scavenging fractions have traditionally been implemented in many GCMs, including ECHAM5HAM, and some models have simply assumed that 100% of the aerosol in a cloud is scavenged into the cloud droplets and ice crystals (e.g., Barth et al., 2000; Chin et al., 2000; Takemura et al., ”
A Multisensor Perspective on the Radiative Impacts of Clouds and Aerosols (2013, methodology): “(1991) and Deepak and Gerber (1983), similar to the models used by the Spectral Radiation-Transport Model for Aerosol Species (SPRINTARS) global transport model (Takemura et al. 2002).”
Direct radiative effect of aerosols as determined from a combination of MODIS retrievals and GOCART simulations (2004, methodology): “Because no details of surface albedo are provided in Takemura et al. [2002] , we cannot quantify such impacts.”
Overview of the Atmospheric Brown Cloud East Asian Regional Experiment 2005 and a study of the aerosol direct radiative forcing in east Asia (2007, methodology): “sensing methods by NASA [Kaufman et al., 2002] and by the four channel algorithm of Higurashi and Nakajima [2002], and the SPRINTARS aerosol and radiation model implemented in the CCSR (Center for Climate System Research, The University of Tokyo)-NIES (National Institute of Environmental Studies, Ja”
Variability of aerosol and spectral lidar and backscatter and extinction ratios of key aerosol types derived from selected Aerosol Robotic Network locations (2005, background): “, 1997b] and is often considered by the climate modeling community [Koch, 2001; Takemura et al., 2002; Yu et al., 2004].”
Monthly Averages of Aerosol Properties: A Global Comparison Among Models, Satellite Data, and AERONET Ground Data (2003, methodology): “CCSR (CC) (or SPRINTARS) from the Center for Climate System Research at the University of Tokyo and from Kyushu University (Tokyo and Kyushu, Japan), is a chemical transport model [Takemura et al., 2000, 2002].”
Wintertime aerosol properties during foggy and nonfoggy days over urban center Delhi and their implications for shortwave radiative forcing (2006, background): “Exact knowledge of single-scattering albedo is very crucial as small error in its magnitude can produce large difference in the estimated values aerosol radiative forcing [ Takemura et al., 2002 ].”
Relative humidity dependence of aerosol optical properties and direct radiative forcing in the surface boundary layer at Xinken in Pearl River Delta of China : An observation based numerical study (2008, background): “…humidification factors, the influences of RH on aerosol radiative properties have been investigated in transport models by assumed or measured xsp for various types of aerosols (Charlson et al., 1991; Chin et al., 2002; Formenti et al., 2002; Takemura et al., 2002, 2006; Markowicz et al., 2003).”
Application of the CALIOP layer product to evaluate the vertical distribution of aerosols estimated by global models: AeroCom phase I results (2012, result): “Following Textor et al. [2007], we compare our results from the AeroCom A experiment (in which models used their own emission data sets), with AeroCom B simulations (in which models used Dentener et al.”
The Non-hydrostatic Icosahedral Atmospheric Model: description and development (2014, methodology): “Currently, NICAM is implemented with a global 3D aerosol transport-radiation model, the Spectral RadiationTransport Model for Aerosol Species (SPRINTARS) (described fully in Takemura et al. 2000, 2002, 2005, 2009; Goto et al. 2011a).”
How much can the vertical distribution of black carbon affect its global direct radiative forcing? (2010, background): “These wereMPI_HAM [Stier et al., 2005], UMI [Liu et al., 2005], SPRINTARS [Takemura et al., 2002], and LSCE [Textor et al., 2006].”