What is it about?
logs of navigation-grade global positioning system (GPS) receivers is used to track the movements of seismic stations situated on moving ice of Antarctica. Results resolve both very slow ice velocities near dome A, East Antarctica, and velocities of >100 m/yr, on Thwaites Glacier in West Antarctica. The results indicate that several months of navigation-grade GPS measurements provide reliable measures of ice sheet movement.
Featured Image
Why is it important?
navigation-grade global positioning system (GPS) receivers can measure ice sheet movement of Antarctica
Perspectives
Read the Original
This page is a summary of: Antarctic ice velocities from GPS locations logged by seismic stations, Antarctic Science, November 2014, Cambridge University Press,
DOI: 10.1017/s0954102014000704.
You can read the full text:
Resources
Contributors
The following have contributed to this page