Climate effects of anthropogenic sulfate: Simulations from a coupled chemistry/climate model
Conference
·
OSTI ID:10108564
In this paper, we use a more comprehensive approach by coupling a climate model with a 3-D global chemistry model to investigate the forcing by anthropogenic aerosol sulfate. The chemistry model treats the global-scale transport, transformation, and removal of SO{sub 2}, DMS and H{sub 2}SO{sub 4} species in the atmosphere. The mass concentration of anthropogenic sulfate from fossil fuel combustion and biomass burning is calculated in the chemistry model and provided to the climate model where it affects the shortwave radiation. We also investigate the effect, with cloud nucleation parameterized in terms of local aerosol number, sulfate mass concentration and updraft velocity. Our simulations indicate that anthropogenic sulfate may result in important increases in reflected solar radiation, which would mask locally the radiative forcing from increased greenhouse gases. Uncertainties in these results will be discussed.
- Research Organization:
- Lawrence Livermore National Lab., CA (United States)
- Sponsoring Organization:
- USDOE, Washington, DC (United States); National Aeronautics and Space Administration, Washington, DC (United States)
- DOE Contract Number:
- W-7405-ENG-48
- OSTI ID:
- 10108564
- Report Number(s):
- UCRL-JC--114078; CONF-940115--15; ON: DE94004352; CNN: NAGW-1287
- Country of Publication:
- United States
- Language:
- English
Similar Records
An assessment of the radiative effects of anthropogenic sulfate
Microphysical and compositional influences on shortwave radiative forcing of climate by sulfate aerosols
The whitehouse effect: shortwave radiative forcing of climate by anthropogenic aerosols
Journal Article
·
Fri Jan 31 23:00:00 EST 1997
· Journal of Geophysical Research
·
OSTI ID:508961
Microphysical and compositional influences on shortwave radiative forcing of climate by sulfate aerosols
Conference
·
Sat Dec 31 23:00:00 EST 1994
·
OSTI ID:126286
The whitehouse effect: shortwave radiative forcing of climate by anthropogenic aerosols
Conference
·
Fri Dec 30 23:00:00 EST 1994
·
OSTI ID:10114550