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Relevant bibliographies by topics / Community Atmospheric Model

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Journal articles

Academic literature on the topic 'Community Atmospheric Model'

Author: Grafiati

Published: 6 September 2023

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Journal articles on the topic "Community Atmospheric Model"

1

Long, M. S., W. C. Keene, R. Easter, et al. "Implementation of the chemistry module MECCA (v2.5) in the modal aerosol version of the Community Atmosphere Model component (v3.6.33) of the Community Earth System Model." Geoscientific Model Development Discussions 5, no. 2 (2012): 1483–501. http://dx.doi.org/10.5194/gmdd-5-1483-2012.

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Abstract. A coupled atmospheric chemistry and climate system model was developed using the modal aerosol version of the National Center for Atmospheric Research Community Atmosphere Model (modal-CAM) and the Max Planck Institute for Chemistry's Module Efficiently Calculating the Chemistry of the Atmosphere (MECCA) to provide enhanced resolution of multiphase processes, particularly those involving inorganic halogens, and associated impacts on atmospheric composition and climate. Three Rosenbrock solvers (Ros-2, Ros-3, RODAS-3) were tested in conjunction with the basic load balancing options av

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2

Long, M. S., W. C. Keene, R. Easter, et al. "Implementation of the chemistry module MECCA (v2.5) in the modal aerosol version of the Community Atmosphere Model component (v3.6.33) of the Community Earth System Model." Geoscientific Model Development 6, no. 1 (2013): 255–62. http://dx.doi.org/10.5194/gmd-6-255-2013.

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Abstract. A coupled atmospheric chemistry and climate system model was developed using the modal aerosol version of the National Center for Atmospheric Research Community Atmosphere Model (modal-CAM; v3.6.33) and the Max Planck Institute for Chemistry's Module Efficiently Calculating the Chemistry of the Atmosphere (MECCA; v2.5) to provide enhanced resolution of multiphase processes, particularly those involving inorganic halogens, and associated impacts on atmospheric composition and climate. Three Rosenbrock solvers (Ros-2, Ros-3, RODAS-3) were tested in conjunction with the basic load-balan

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3

Chen, Yong, Yong Han, Quanhua Liu, Paul Van Delst, and Fuzhong Weng. "Community Radiative Transfer Model for Stratospheric Sounding Unit." Journal of Atmospheric and Oceanic Technology 28, no. 6 (2011): 767–78. http://dx.doi.org/10.1175/2010jtecha1509.1.

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Abstract To better use the Stratospheric Sounding Unit (SSU) data for reanalysis and climate studies, issues associated with the fast radiative transfer (RT) model for SSU have recently been revisited and the results have been implemented into the Community Radiative Transfer Model version 2. This study revealed that the spectral resolution for the sensor’s spectral response functions (SRFs) calculations is very important, especially for channel 3. A low spectral resolution SRF results, on average, in 0.6-K brightness temperature (BT) errors for that channel. The variations of the SRFs due to

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4

Baumgaertner, A. J. G., P. Jöckel, A. Kerkweg, R. Sander, and H. Tost. "Implementation of the Community Earth System Model (CESM) version 1.2.1 as a new base model into version 2.50 of the MESSy framework." Geoscientific Model Development 9, no. 1 (2016): 125–35. http://dx.doi.org/10.5194/gmd-9-125-2016.

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Abstract. The Community Earth System Model (CESM1), maintained by the United States National Centre for Atmospheric Research (NCAR) is connected with the Modular Earth Submodel System (MESSy). For the MESSy user community, this offers many new possibilities. The option to use the Community Atmosphere Model (CAM) atmospheric dynamical cores, especially the state-of-the-art spectral element (SE) core, as an alternative to the ECHAM5 spectral transform dynamical core will provide scientific and computational advances for atmospheric chemistry and climate modelling with MESSy. The well-established

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5

Blackmon, Maurice, Byron Boville, Frank Bryan, et al. "The Community Climate System Model." Bulletin of the American Meteorological Society 82, no. 11 (2001): 2357–76. http://dx.doi.org/10.1175/1520-0477(2001)082<2357:tccsm>2.3.co;2.

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6

Collins, William D., Philip J. Rasch, Byron A. Boville, et al. "The Formulation and Atmospheric Simulation of the Community Atmosphere Model Version 3 (CAM3)." Journal of Climate 19, no. 11 (2006): 2144–61. http://dx.doi.org/10.1175/jcli3760.1.

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Abstract A new version of the Community Atmosphere Model (CAM) has been developed and released to the climate community. CAM Version 3 (CAM3) is an atmospheric general circulation model that includes the Community Land Model (CLM3), an optional slab ocean model, and a thermodynamic sea ice model. The dynamics and physics in CAM3 have been changed substantially compared to implementations in previous versions. CAM3 includes options for Eulerian spectral, semi-Lagrangian, and finite-volume formulations of the dynamical equations. It supports coupled simulations using either finite-volume or Eule

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7

Pedatella, N. M., H. L. Liu, and A. D. Richmond. "Atmospheric semidiurnal lunar tide climatology simulated by the Whole Atmosphere Community Climate Model." Journal of Geophysical Research: Space Physics 117, A6 (2012): n/a. http://dx.doi.org/10.1029/2012ja017792.

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8

Bonan, Gordon B., Keith W. Oleson, Mariana Vertenstein, et al. "The Land Surface Climatology of the Community Land Model Coupled to the NCAR Community Climate Model*." Journal of Climate 15, no. 22 (2002): 3123–49. http://dx.doi.org/10.1175/1520-0442(2002)015<3123:tlscot>2.0.co;2.

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9

Sander, Rolf, Andreas Baumgaertner, David Cabrera-Perez, et al. "The community atmospheric chemistry box model CAABA/MECCA-4.0." Geoscientific Model Development 12, no. 4 (2019): 1365–85. http://dx.doi.org/10.5194/gmd-12-1365-2019.

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Abstract. We present version 4.0 of the atmospheric chemistry box model CAABA/MECCA that now includes a number of new features: (i) skeletal mechanism reduction, (ii) the Mainz Organic Mechanism (MOM) chemical mechanism for volatile organic compounds, (iii) an option to include reactions from the Master Chemical Mechanism (MCM) and other chemical mechanisms, (iv) updated isotope tagging, and (v) improved and new photolysis modules (JVAL, RADJIMT, DISSOC). Further, when MECCA is connected to a global model, the new feature of coexisting multiple chemistry mechanisms (PolyMECCA/CHEMGLUE) can be

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10

Jochum, Markus, Alexandra Jahn, Synte Peacock, et al. "True to Milankovitch: Glacial Inception in the New Community Climate System Model." Journal of Climate 25, no. 7 (2012): 2226–39. http://dx.doi.org/10.1175/jcli-d-11-00044.1.

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Abstract The equilibrium solution of a fully coupled general circulation model with present-day orbital forcing is compared to the solution of the same model with the orbital forcing from 115 000 years ago. The difference in snow accumulation between these two simulations has a pattern and a magnitude comparable to the ones inferred from reconstructions for the last glacial inception. This is a major improvement over previous similar studies, and the increased realism is attributed to the higher spatial resolution in the atmospheric model, which allows for a more accurate representation of the

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