Frozen Mars North Pole Ice Patterns Observed by HiRISE
Written by Ian O'Neill
As the Phoenix Mars lander will agree, it's cold near Mars' North Pole. Phoenix
is currently
seeing the winter frost encroach on its location, bright patches of ice
appearing on the
rocks surrounding it. Another sure sign of winter at this high latitude is the
loss of light;
soon day will turn to night, forcing Phoenix to enter a Sun-deprived coma. But
as one
Mars mission draws to a close, other missions continue their diligent watch over
the
planet 24/7. One such mission is NASA's Mars Reconnaissance Orbiter (MRO), using
its
High Resolution Imaging Science Experiment (or HiRISE for short) to pick out the
tiny
surface features on the Red Planet from around 320 km (200 miles) above.
As winter sets in on the Martian northern hemisphere, HiRISE continues to
capture some
stunning images of the translucent icy surface…
Mars dune detail showing the southwesterly dominant wind direction
(NASA/JPL/HiRISE)
These images were acquired at the end of August by HiRISE, and it is evident
there was
plenty of ice on the surface of this northern region. The MRO was making a pass
over a
geographical latitude of 77° when these pictures were taken, capturing the
complex
cracking of translucent surface ice, contrasting with the dark sand of a vast
number of
barchan dunes, a feature we often observe on Earth as well as on Mars. Phoenix
landed at
68° latitude, a little further south than these HiRISE images, but it can be
seen there is a
lot more ice for that time of the year only 10° further north of Phoenix's
location (after all,
no surface frost was observed by the lander in August).
It is thought that the bright areas of ice in the image above comes from surface
frost
deposited the previous year, but the polar temperatures remained so cold
throughout the
Martian summer that the frost didn't sublimate into the thin atmosphere. So, the
surface
ice remained throughout the year, gradually undergoing physical changes,
creating a
polygonal texture when viewed from orbit. The texture was probably down to
temperature
variations, stressing and cracking the ice.