HR: 09:00h
AN: A51F-07 [Abstracts]
TI: The modelled impact of changes in the CO2 concentration on the middle and upper atmosphere: sensitivity to gravity wave activity and parameterization
AU: * Cnossen, I
EM: ic35@ion.le.ac.uk
AF: Radio and Space Plasma Physics Group, University of Leicester, University Road,
Leicester, LE1 7RH, United Kingdom
AU: Arnold, N
EM: nfa1@ion.le.ac.uk
AF: Radio and Space Plasma Physics Group, University of Leicester, University Road,
Leicester, LE1 7RH, United Kingdom
AU: Harris, M
EM: matthew@apl.ucl.ac.uk
AF: Atmospheric Physics Laboratory, University College London, Gower Street, London, WC1E
6BT, United Kingdom
AU: Yigit, E
EM: erdal@apl.ucl.ac.uk
AF: Atmospheric Physics Laboratory, University College London, Gower Street, London, WC1E
6BT, United Kingdom
AB:
Cooling of the middle and upper atmosphere by CO2 is dependent on the temperature of the ambient
atmosphere. Since the temperature structure is partly controlled by the residual circulation, driven mostly by the
dissipation of gravity waves, CO2 cooling is expected to be dependent on the strength of the residual
circulation, and thereby on the gravity wave activity. Also, the dissipation process of gravity waves is dependent on
the temperature of the atmosphere they are propagating through, and this dependence is reflected differently in
different gravity wave parameterization schemes. This may have important consequences for temperature trends
due to changes in the CO2 concentration as calculated by middle and upper atmospheric GCMs. Therefore
we will show, using the Coupled Middle Atmosphere and Thermosphere model 2 (CMAT2), how such trends
depend on the gravity wave parameterization that is used and the gravity wave activity that is assumed by the
model.
DE: 0325 Evolution of the atmosphere (1610, 8125)
DE: 0340 Middle atmosphere: composition and chemistry
DE: 0341 Middle atmosphere: constituent transport and chemistry (3334)
DE: 0350 Pressure, density, and temperature
DE: 0355 Thermosphere: composition and chemistry
SC: Atmospheric Sciences [A]
MN: 2007 Fall Meeting