Simulation experiments performed with MOGUNTIA so far:
Desert dust
Radioactive gases
Chemical tracers
More detail :
Sources: Industrial nations (Spray cans, air conditioning, ...) 90% Northern Hemisphere. Pretty well known annual amounts and global distribution.
Sink: Mixing into the stratosphere.
Aim of research: Long time (~50ys) large scale transport simulation, interhemispheric exchange, stratospheric exchange.
Publications: Zimmermann, 1988.
Sources: Nuclear recycling plants, Northern Hemisphere. Pretty well known annual amounts and global distribution.
Sink: Radioactive decay (halflife ~10y).
Aim of research: Source receptor studies, interhemispheric exchange, longtime simulation, boundary layer parameterisation.
Publications: Zimmermann et al., 1989.
Sources: soils.
Sink: Radioactive decay (halflife ~1.8d).
Aim of research: Subgrid scale transport, cumulus convection.
Publications: Feichter and Crutzen, 1990.
Sources: clouds.
Sink: (in preparation).
Aim of research: Night time removal of ozone by NO2 reaction on aerosol.
Publications: Dentener and Crutzen, 1993.
Sources: Industrial combustion processes.
Sink: OH- oxidation.
Aim of research: (in preparation).
Publications: Zimmermann, 1988, Kanakidou et al., 1993.
Sources: cf. 1.
Sink: OH- oxidation (OH precalculated by 2D-model or by
MOGUNTIA
ozone chemistry simulation ), small
ocean take up.
Aim of research: Testing the oxidation capacity of the troposphere, resp. The validity of a calculated OH distribution, i.e. its global distribution and seasonality.
Publications: Zimmermann, 1988; Kanakidou et al., 1993.
Sources: Stratosphere and photochemistry.
Sink: Photochemistry (day time), NO2 reaction (night time).
Aim of research:
Species:
Mineral aerosol (primary aerosol).
Sources: Wind-blown soils.
Sink: Gravitational settling, dry deposition at surface, and wet scavenging.
Aim of research: The role of mineral aerosol as a reactive surface in tropospheric air chemistry.
Publications: Dentener et al., 1997.
2