 |
|
|
GMI Home > Model Evaluation
Model Evaluation
Grading Model Performance
Physically-based model evaluation is an essential element of all
GMI work. We have developed a variety of methods for evaluating
and grading model performance in the stratosphere. These methods
have been described in several GMI publications (Douglass et al.,
1999; Strahan and Douglass, 2004; and Douglass et al., 2004), which
can be found under GMI Publications.
The diagnostics presented here are part of a larger effort to
evaluate chemistry-climate models (CCMs). The Chemistry-Climate
Validation Activity for SPARC (CCMVal) is project that addresses
the need for consistent evaluation/validation of CCMs with detailed
descriptions of the stratosphere. Participants in CCMVal have developed
a number of diagnostics for stratospheric dynamics, transport,
chemistry, and radiation. Please visit the CCMVal
Evaluation Table for a complete listing of the diagnostics.
In this section, you can download model diagnostics packages.
Each package contains the necessary data sets, IDL routines,
and instructions for applying the diagnostic to your own model
results.
Model
Diagnostic Tests
1. The Antartic
Vortex Transport and Mixing Test
 |
This diagnostic examines a model’s ability
to produce and maintain the dynamical barrier to transport
found at the edge of the lower stratospheric Antarctic vortex
in spring. The presence of a realistic vortex edge is important
for containment of chemical perturbed air and the simulation
of O3 loss. This diagnostic is described in detail
in Strahan and Douglass [2004].
Required data set: This test uses 12 years of HALOE
CH4 and temperature measurements between 44oS-80oS
from September 1 through November 30. Data from 2002 is excluded
because of the unusually early vortex breakup. HALOE temperature
measurements are used to interpolate the CH4 observations
to isentropic surfaces. Probability distribution functions
are calculated on the two potential temperature surfaces
for 6 space-time bins: for each of the 3 months (Sep, Oct,
Nov), there is one bin each for the latitude ranges 44-60oS
and 60-80oS. Because of the low interannual variability
in southern hemisphere dynamics, it is feasible to combine
the measurements from 12 years of observations. HALOE’s
sparse sampling (15 profiles around a latitude circle per
day) prohibits the calculation of meaningful PDFs from a
single year’s data.
You may download this ‘processed’ data set from
this web page. The data file containing HALOE pdfs was created
in IDL by the ‘save’ command. It can be read
into an IDL session using the ‘restore’ command.
This data file contains HALOE CH4 on seven isentropic
surfaces (450, 600, 800, 1000, 1200, 1400, 1600K), although
the ‘official’ test only includes the lowest
two levels. |
If you are unable to
use IDL data sets, please contact Susan
Strahan for data in an alternative format.
Analysis software: There are several IDL procedures that
you may download for the calculation of PDFs from your model output.
The routine requires model output on a regular grid. Please read
the comments inside ‘calc_model_pdf.pro’ for
more detailed instructions. This procedure calls a number of other
IDL procedures, all of which are available here.
Download this test: You may download a detailed
description of this test and an example
of how to grade a model with this test.
There are 6 required IDL routines and 2 IDL savesets with the
necessary HALOE data. They have been tarred together and can
be downloaded here.
| Top
of Page |
|
|