Hubble Space Telescope (HST) Model Images of Mars

First, here is a web site with lots of neat HST images of Mars. Now, here is one of our models: Cool, huh? We took a surface reflectance map at a wavelength of 1042 nanometers from Bell et al. (1997 JGR, 102, 9109-9124). The model atmosphere has a dust optical depth of 0.4. Subsolar and Subearth points are arbitrarily chosen to be (lat=25 deg.,lon=80) and (lat=25,lon=40) respectively.

An example of an initial study we are undertaking is to model atmospheric Ozone abundances of Mars by comparing models to HST images taken in the Hartley band (255 nm). Below is a model of the martian atmosphere that contains carbon dioxide (CO2) and ozone (O3) at a wavelength of 255 nanometers. As the ozone absorption increases to the right, the mars disk gets slightly darker. The image on the far right is a 3-color (Blue Green Red) combination of the images on the left. It's mostly blue because the first image is much brighter than the other two. Note, these are run at the same spatial resolution as HST WFPC2 camera, but they haven't been convolved with the HST point-spread-function. Note also that we use a constant surface albedo so there are no surface features in these models.

Varying Ozone (O3) levels

 O3 (micron-atm)  0 2 4
 ave albedo  1 0.37 0.23
 normal optical depth  0.064  0.121  0.179

Here's pixel-wide slices across the surface of the disks of the 3 images, just showing the limb area. The images were convolved with a voigt function that resembles HST PSF, before slicing.


Our study will focus on the limb, that is, the outer edge of the atmosphere, where we can see a large effect and as affected from the uncertainties of the surface properties. The multi-year coverage of the HST data (1995-7) will provide information about the latitudinal, seasonal, and interannual variations of Martian ozone column densities. We will focus our efforts on the period from late spring through the end of summer (in the northern hemisphere), with special attention given to low-to-mid latitude regions where the knowledge is very incomplete.

return to B. Whitney's Mars page
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