Mars has permanent polar caps at both the North and South poles. They are composed of water ice and CO2 ice. One component of the polar caps is sesaonal, meaning it comes and goes depending on the season. The other component is permanent, and never completely vanishes. The permanent cap over the South Pole is made of CO2 ice, while the permanent cap over the North Pole is made of H2O ice and is much larger.

South Polar Cap as seen by Viking
At high resolution, the permanent caps are composed of many layers of terrain, probably due to the long-term history of deposition of frost and dust onto the surface. By studying these layers, planetary scientists can learn something about long-term climate changes on Mars.

Image of North Polar Cap layered terrain, courtesy of Malin Space Science Systems/NASA, from Mars Global Surveyor
With increased exploration of the Martian surface with improved technology on our current spacecraft, we see more and more evidence for liquid water flowing (in the past) on Mars' surface. Two examples are shown below.
Gullies that resemble river gullies on Earth:

Image courtesy of Malin Space Science Systems/NASA, from Mars Global Surveyor
Outflow patterns on the walls of the South Polar region:


Left: Viking context image. Right: image courtesy of Malin Space Science Systems/NASA, from Mars Global Surveyor
Runoff channels:

These runoff channels are actually on Earth! This image, taken from space, shows a region of Yemen, which is now a desert. This is evidence for climate changes that have occurred on Earth. After the last Ice Age, Yemen was a more temperate grassland. The climate is much more arid today.
We will now discuss the changes that occurred in the Martian climate. What happened to all of the water? We will use the article you read from Sky and Telescope, entitled "The Iceball Next Door," as a starting point for our discussion.
Break into groups of 3-5 people, and in 10 minutes, be prepared to discuss the following questions:
From "Taking a Global Inventory"