Jb. Pollack et al., SIMULATIONS OF THE GENERAL-CIRCULATION OF THE MARTIAN ATMOSPHERE .2. SEASONAL PRESSURE VARIATIONS, J GEO R-PLA, 98(E2), 1993, pp. 3149-3181
We have simulated the CO2 seasonal cycle of the Martian atmosphere and
surface with a hybrid energy balance model that incorporates dynamica
l and radiation information from a large number of general circulation
model (GCM) runs. This information includes heating due to atmospheri
c heat advection, the seasonally varying ratio of the surface pressure
at the two Viking landing sites to the globally averaged pressure (r(
k)), the rate of CO2 condensation in the atmosphere, and solar heating
of the atmosphere and surface. The GCM runs collectively covered a fu
ll set of seasonal dates and a large range of dust optical depths. We
have compared the predictions of the energy balance model with the sea
sonal pressure variations measured at the two Viking landing (VL) site
s and the springtime retreat of the seasonal polar cap boundaries. Num
erical experiments with the energy balance model indicate that the fol
lowing quantities have a strong influence on the VL seasonal pressures
: albedo A(is) of the seasonal CO2 ice deposits, emissivity e(is) of t
his deposit, atmospheric heat advection, and the pressure ratio r(k).
This last factor does not enter into the seasonal CO2 condensation/sub
limation cycle in a significant way. The numerical experiments also in
dicate that the following factors have only a minor effect on the VL p
ressures: (1) the net radiative effects (solar plus thermal) of atmosp
heric dust at the latitudes of the polar caps, and (2) the subsurface
heat conduction. The significant influence of the pressure ratio r(k)
on the VL, seasonal pressures is due to large seasonal variations in t
he global distribution of surface pressure. At low and mid-latitudes,
these ''weather'' variations are engendered by seasonal changes in the
Hadley circulation and by seasonal changes in the atmospheric scale h
eight close to the surface. Comparison of the VL1 and VL2 pressures wi
th one another provide direct evidence for the presence of such a ''we
ather component'' in the measured pressures. The differential weather
component (VL2-VL1) derived from the data is reproduced approximately
by the energy balance model. We find that the seasonal weather variati
ons account for about 20% and 30% of the seasonal pressure variations
measured at VL1 and VL2, respectively, that dynamical and scale height
variations make comparable contributions to the weather component dur
ing years without global dust storms, and that the dynamical contribut
ion is the larger one during years with global dust storms. Interannua
l variations in the weather component, rather than variations in CO2 c
ondensation rates, are the dominant sources of the observed interannua
l variations of pressure during the season of global dust storms. Opti
mum fits to the Viking pressure measurements and the data on the polar
cap boundaries are achieved with values of about 0.45 and 0.75 for A(
is) and e(is), respectively. The former value is consistent with avail
able photometric determinations of the albedo of the seasonal caps, wh
ile the latter value, especially in light of infrared thermal mapper b
rightness temperatures at high latitudes, may reflect, in part, the in
fluence of the polar hood on the radiation balance of the winter polar
regions.