2012
DOI: 10.5194/gmd-5-369-2012
|View full text |Cite
|
Sign up to set email alerts
|

CAM-chem: description and evaluation of interactive atmospheric chemistry in the Community Earth System Model

Abstract: We discuss and evaluate the representation of atmospheric chemistry in the global Community Atmosphere Model (CAM) version 4, the atmospheric component of the Community Earth System Model (CESM). We present a variety of configurations for the representation of tropospheric and stratospheric chemistry, wet removal, and online and offline meteorology. Results from simulations illustrating these configurations are compared with surface, aircraft and satellite observations. Major biases include a negative bias in … Show more

Help me understand this report
View preprint versions

Search citation statements

Order By: Relevance

Paper Sections

Select...
3
1
1

Citation Types

23
703
1

Year Published

2013
2013
2018
2018

Publication Types

Select...
8
2

Relationship

1
9

Authors

Journals

citations
Cited by 699 publications
(727 citation statements)
references
References 97 publications
23
703
1
Order By: Relevance
“…Weak emission lines in this frequency range due to trace species such as nitric oxide and nitrogen dioxide are not included in our wind retrieval calculations. Winter (June, July, August -JJA) and summer (December, January, February -DJF) seasonal average profiles of O 3 , CO, water vapour, O 2 , and temperature over the altitude range 0-120 km are calculated from 12 years of simulations by the Whole Atmosphere Community Climate Model with Specified Dynamics (SD-WACCM) version 3.5.48 (Garcia et al, 2007;Marsh, 2011;Lamarque et al, 2012). The profiles, calculated by combining the day-time and night-time SD-WACCM profiles at 74.8 and 76.7 • S, the gridded latitudes closest to Halley, according to the solar elevation angle at 72 km are shown in Fig.…”
Section: Atmospheric Spectramentioning
confidence: 99%
“…Weak emission lines in this frequency range due to trace species such as nitric oxide and nitrogen dioxide are not included in our wind retrieval calculations. Winter (June, July, August -JJA) and summer (December, January, February -DJF) seasonal average profiles of O 3 , CO, water vapour, O 2 , and temperature over the altitude range 0-120 km are calculated from 12 years of simulations by the Whole Atmosphere Community Climate Model with Specified Dynamics (SD-WACCM) version 3.5.48 (Garcia et al, 2007;Marsh, 2011;Lamarque et al, 2012). The profiles, calculated by combining the day-time and night-time SD-WACCM profiles at 74.8 and 76.7 • S, the gridded latitudes closest to Halley, according to the solar elevation angle at 72 km are shown in Fig.…”
Section: Atmospheric Spectramentioning
confidence: 99%
“…4, we describe the satellite observations by MODIS and CALIOP that are used to evaluate the different model simulations and put the outcome of this modelling exercise into perspective. (Lamarque et al, 2012). Additionally, the model does not include indirect aerosol effects as a result of changing aerosol concentrations, because cloud formation is based on fixed CCN concentrations which only differentiate between relatively clean air above oceans and more polluted air over land masses.…”
Section: Model Descriptionmentioning
confidence: 99%
“…WACCM has a specified dynamics version named SD-WACCM (Lamarque et al, 2012;Kunz et al, 2011) which is suitable for intercomparisons with measurement data. SD-…”
Section: Sd-waccmmentioning
confidence: 99%