Saturday 3 December 2016

Shadow of Rosetta on Comet 67P



This week’s “guess the planet” image comes from comet 67P/Churyumov-Gerasimenko. Credit for this image goes to ESA’s Rosetta Team.

Rather than talking about the geology in this image I drew your attention to the dark smudge like feature in the bottom part of the image. This feature is entirely man made as it is actually the shadow of the Rosetta spacecraft, cast on the surface of the comet during a close flyby in 2015. ESA report that the shadow is 20 by 50 metres, indicating the scale of the image.

At the time this image was taken the Rosetta orbiter came within six kilometres of the comet’s surface allowing it to take images of an unprecedentedly high resolution. As ESA outline on their website the fact that the spacecraft is casting a shadow during its close approach is also very significant. This means that Rosetta was passing between the comet and the sun, and thus the sun was directly overhead. 

This meant that the surface features didn’t cast shadows across the image and allowed the Rosetta team to determine the reflectance of the materials which make up the comets surface. As planetary scientists we are often interested in the “albedo” of a surface. This is the proportion of light which it reflects, and can tell us a lot about the sort of materials the surface is made of. However the lighting conditions at the time an image is taken will have just as much of an effect on the brightness of an imaged surface as its albedo. Because there are few shadows in this image (apart from the obvious one) the Rosetta team know that the reflectance of the surface materials reflects their true albedo. 

The angle of the sun is very important when examining remote sensing images. A couple of weeks ago I talked about how you can use the direction of shadows to distinguish between positive and negative relief features. The length of shadows can also be used to add a third dimension to what would otherwise be a flat image. So long as you know the angle of the sun you can use some basic trigonometry to determine the height of the feature casting the shadow. 

The sun is thus a very useful tool in interpreting the surface of another planet. 

Image credit: ESA/Rosetta/NAVCAM – CC BY-SA IGO 3.0

The Original image, and information about it's properties can be found here:

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