A Diagnostic part of the SPARC Chemistry-Climate Model
Validation Activity CCMVal
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Useful
information on subtropical and polar mixing barriers can be obtained
from instantaneous snapshots of tracer fields,
which makes the model-measurement comparison straightforward. For this
purpose
there is a wealth of high-quality observational data available. A
simple check
on the degree of isolation is provided by the sharpness of latitudinal
gradients of long-lived species (CH4, N2O,
CFC-11).
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Figure 1. Climatological zonal-mean CH4 mixing ratios from the CCMs and HALOE in ppmv. Latitudinal profiles at 50 hPa in March (left) and October (right). The grey area shows HALOE plus and minus 1 standard deviation (s) about the climatological zonal mean (from Eyring et al., 2006, their Figure 5). | Figure 2. Absolute
value of the zonal-mean latitudinal gradient of N2O for October in the
CMAM model. The dark colors show low latitudinal gradients of N2O,
while the bright colors show large latitudinal gradients representing
jumps in the mixing ratio across a mixing barrier (from Sankey and
Shepherd, 2003, their Figure 7) |
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