Earth Imaging Journal: Remote Sensing, Satellite Images, Satellite Imagery
Breaking News
Seisland Surveys Wins Esri Canada’s Award of Excellence in GIS
CALGARY, Esri Canada User Conference, May 29, 2015 —...
MEMSIC to Showcase its Latest Sensing Solutions at Sensors Expo and Conference 2015
Andover, MA, May 29, 2015 — MEMSIC, Inc. plans to...
Register now – it’s Pivotal
May 29, 2015 — We have been busy curating...
New Mapping Agreement to Benefit United Kingdom and Ireland Location Data Users
May 29, 2015 — A new three party agreement...
NOAA: Below-normal Atlantic Hurricane Season is Likely this Year
May 27, 2015—NOAA’s Climate Prediction Center says the 2015...

An Earth-orbiting radar can’t see the ocean floor, but it can measure ocean-surface height variations induced by the ocean floor’s topography. When interesting features are discovered in satellite measurements, they later can be surveyed in fine detail by ships.

CryoSat was designed to measure Arctic sea-ice thickness, but high-resolution mapping of ocean-floor topography now is being added to the ice mission’s repertoire.

The main objective of the polar-orbiting CryoSat is to measure the thickness of polar sea ice and monitor changes in the ice sheets that blanket Greenland and Antarctica. But the satellite’s radar altimeter can detect tiny variations in the height of the ice as well as measure sea level.

The topography of the ocean surface mimics the rises and dips of the ocean floor due to the gravitational pull. Areas of greater mass, such as underwater mountains, have a stronger pull, attracting more water and producing a minor increase in ocean-surface height. Therefore, instruments that measure sea-surface height incidentally map the ocean floor in previously uncharted areas.

Read the full story.

Image courtesy of Scripps Institution of Oceanography.

 

Comments are closed.