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An improvement on the dust emission scheme in the global aerosol-climate model ECHAM5-HAM, Atmos (2008)

by T Cheng, Y Peng, J Feichter, I Tegen
Venue:Chem. Phys
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Atmospheric Chemistry and Physics Simulation of mineral dust aerosol with Piecewise Log-normal Approximation (PLA) in CanAM4-PAM

by Y. Peng, K. Von Salzen, J. Li , 2012
"... Abstract. A new size-resolved dust scheme based on the numerical method of piecewise log-normal approximation (PLA) was developed and implemented in the fourth gener-ation of the Canadian Atmospheric Global Climate Model with the PLA Aerosol Model (CanAM4-PAM). The total simulated annual global dust ..."
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Abstract. A new size-resolved dust scheme based on the numerical method of piecewise log-normal approximation (PLA) was developed and implemented in the fourth gener-ation of the Canadian Atmospheric Global Climate Model with the PLA Aerosol Model (CanAM4-PAM). The total simulated annual global dust emission is 2500 Tg yr−1, and the dust mass load is 19.3 Tg for year 2000. Both are consis-tent with estimates from other models. Results from simula-tions are compared with multiple surface measurements near and away from dust source regions, validating the genera-tion, transport and deposition of dust in the model. Most dis-crepancies between model results and surface measurements are due to unresolved aerosol processes. Biases in long-range transport are also contributing. Radiative properties of dust aerosol are derived from approximated parameters in two size modes using Mie theory. The simulated aerosol optical depth (AOD) is compared with satellite and surface remote sensing measurements and shows general agreement in terms of the dust distribution around sources. The model yields a dust AOD of 0.042 and dust aerosol direct radiative forc-ing (ADRF) of −1.24 W m−2 respectively, which show good consistency with model estimates from other studies. 1
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...e in the model. A global map of surface aerodynamic roughness length is obtained from an analysis of measurements with the European Remote Sensing (ERS) satellite scatterometer (Prigent et al., 2005; =-=Cheng et al., 2008-=-) and included in the model as a climatological input field. Arid and semi-arid regions with high surface roughness require a large U∗th to uplift soil particles. Because rough surface protects partic...

Bay of Bengal and the Arabian Sea region during ICARB using

by R. Cherian, C. Venkataraman, S. Ramach, J. Quaas, S. Kedia , 2012
"... Examination of aerosol distributions and radiative effects over the ..."
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Examination of aerosol distributions and radiative effects over the
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... of ECHAM5.5-HAM, global soil textures were prescribed for preferential source regions (Tegen et al., 2002), which results in a significant underestimate of the dust emission flux over Asian regions (=-=Cheng et al., 2008-=-). Alternate approaches, e.g. reflectivity-based soil erodibility factor (Grini et al., 2005), which show better agreement of dust flux with measurements, might improve dust parameterization in ECHAM5...

© Author(s) 2012. CC Attribution 3.0 License. Atmospheric Chemistry and Physics The isotopic record of Northern Hemisphere atmospheric carbon monoxide since 1950: implications for the CO budget

by Z. Wang, P. Martinerie, K. Park, V. Petrenko, E. Witrant, L. K. Emmons, T. Blunier, C. A. M. Brenninkmeijer, J. E. Mak , 2012
"... doi:10.5194/acp-12-4365-2012 ..."
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doi:10.5194/acp-12-4365-2012

Table of contents

by Katja Schmieder, Katja Brödner, Konstanze Kunze, Kerstin Müller, Claudia Peter, Heike Scherf, Editorial Board, Jost Heintzenberg, Hartmut Herrmann, Andreas Macke, Eberhard Renner , 2008
"... Photo and illustration credits © IfT; all pages, except for pages: ..."
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Photo and illustration credits © IfT; all pages, except for pages:

Atmospheric Chemistry and Physics Global dust model intercomparison in AeroCom phase I

by J. Penner, J. Perlwitz, P. Stier, T. Takemura, C. S. Zender
"... doi:10.5194/acp-11-7781-2011 ..."
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doi:10.5194/acp-11-7781-2011
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... or from the weights of filter samples ashed at 500 ◦C after extracting soluble components with water. This database has been largely used for the evaluation of dust models (e.g. Ginoux et al., 2001; =-=Cheng et al., 2008-=-; Tegen et al., 2002) and in the reports of the Intergovernmental Panel of Climate Change (IPCC) of 2001 and 2007. The measurements were taken for the most part in the 1980s and 1990s with varying mea...

ECHAM5-HAMMOZ

by L. Pozzoli, G. Janssens-maenhout, T. Diehl, I. Bey, M. G. Schultz, J. Feichter, E. Vignati, F. Dentener , 2011
"... doi:10.5194/acp-11-9563-2011 ..."
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doi:10.5194/acp-11-9563-2011

Atmospheric Chemistry and Physics The Mineral Dust Cycle in EMAC 2.40: sensitivity to the spectral resolution and the dust emission scheme

by A. Kerkweg, H. Wernli , 2012
"... Abstract. This first detailed analysis of the mineral dust cycle in the ECHAM5/MESSy Atmospheric Chemistry (EMAC) model system investigates the performance of two dust emission schemes, following the approach of Balkanski et al. (2004) and Tegen et al. (2002), respectively, and the influence of the ..."
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Abstract. This first detailed analysis of the mineral dust cycle in the ECHAM5/MESSy Atmospheric Chemistry (EMAC) model system investigates the performance of two dust emission schemes, following the approach of Balkanski et al. (2004) and Tegen et al. (2002), respectively, and the influence of the horizontal model resolution. Here the spec-tral resolutions T42, T63, T85, and T106 are investigated. A basic sulphur chemistry, enabling the coating of insoluble dust particles to make them soluble, is employed in order to realistically describe the ageing and wet deposition of min-eral dust. Independent of the dust emission scheme the five-year simulations with the horizontal resolutions T42 and T63 produce unrealistically high emissions at some grid points in the Tarim Basin in Central Asia, leading to very high dust loads in polar regions. With these coarse resolutions, dust
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...n fluxes of the single size classes are summed up to get a bimodal dust emission with an insoluble accumulation mode (mmr= 0.37 µm, σ = 1.59 µm) and an insoluble coarse mode (mmr= 1.75 µm, σ = 2 µm) (=-=Cheng et al., 2008-=-). As an example the values of the input fields of two prominent dust source regions, the Bodélé Depression in Chad and the Thar Desert in North-West-India, are shown in Table 1. With BK 10-m wind s...

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