What is Parallax?
Parallax is the apparent difference in the location of an object based on point of view. With satellite data this is always something important to consider, because the features you see may not actually be where they appear. This is the first of a three part series focused on the parallax problem. This introduction will review orbital characteristics of the two most common types of meteorological satellites with very different parallax issues. The next two parts will describe those issues in greater detail.
Satellites and Their Types
The full disk Infrared (IR) image above is an example of the earth view as seen by the current GOES satellite with Alaska very close to the northern edge. Mapping that GOES IR imagery to a polar stereographic view focused on Alaska (left) doesn’t actually look that bad from a distance, despite the large angle.
Polar satellites orbit over the poles at a substantially lower altitude, around 850 kilometers or 525 miles, and at a much faster speed. It takes around 100 minutes for a polar satellite to complete one full orbit around the earth. As the earth turns below it, the swath of each pass covers an area just to the west of the previous pass. There is usually some overlap with successive passes that is dependent on latitude and the width of the swath. Polar regions have more frequent overlapping coverage since the orbital tracks always pass near the poles.
By Carl Dierking