Global three‐dimensional simulation of aerosol optical thickness distribution of various origins

By Toshihiko Takemura, Hajime Okamoto, Y. Maruyama, A. Numaguti, A. Higurashi, Teruyuki Nakajima. 2000

445 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/3d1e592e26e856f9d29d7d6d2e16d483660d23ec

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Citations in the corpus

Analysis and quantification of the diversities of aerosol life cycles within AeroCom (2005, unknown): “(1999) interactively (Gillette, 1978; Takemura et al., 2000) interactively (Erickson et al.”
Latitudinal distribution of diazotrophs and their nitrogen fixation in the tropical and subtropical western North Pacific (2009, methodology): “Aeolian dust deposition—Deposition rates of soil dust, including both dry and wet deposition, were estimated by the numerical model, Spectral Radiation–Transport Model for Aerosol Species (SPRINTARS; Takemura et al. 2000).”
Asian dust transported one full circuit around the globe (2009, methodology): “The transport path of the TK1 dust tracked by the CALIOP and the National Institute for Environmental Studies (NIES) ground-based Lidar Network over East Asia is quite consistent with the simulation result of the global aerosol transport model, Spectral Radiation–Transport Model for Aerosol Specie”
Single-Scattering Albedo and Radiative Forcing of Various Aerosol Species with a Global Three-Dimensional Model (2002, methodology): “These ratios are also assumed for the in-cloud coefficients used in the wet deposition process [Takemura et al. 2000, Eq.”
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”
The aerosol-climate model ECHAM5-HAM (2004, methodology): “A number of studies, (e.g. Tegen et al., 1997; Jacobson, 2001; Takemura et al., 2000), incorporated partly size-segregated aerosol modules with several components into global aerosol models, neglecting the microphysical interaction among the components.”
Tropospheric aerosol optical thickness from the GOCART model and comparisons with satellite and sun photometer measurements (2002, methodology): “This conclusion is consistent with the study by Takemura et al. (2000).”
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).”
Sulfur, sea salt, and radionuclide aerosols in GISS ModelE (2006, methodology): “The model sea salt at Samoa is too high in wintertime, similar to sites further to the south in the SH. The model of Takemura et al. [2000] was more successful at simulating the sea-salt amount at Barbados; however, their observations are lower than ours, perhaps based on different years.”
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].”
Incorporating the effect of small‐scale circulations upon dust emission in an atmospheric general circulation model (2004, background): “…model plume is located around 15 N, 5 –10 too far north according to satellite retrievals [Husar et al., 1997; Herman et al., 1997], although the discrepancy could be due to aerosol loading by biomass burning south of 15 N, included in the retrievals [Tegen and Fung, 1994; Takemura et al., 2000].”