Type of geospatial technology
Remote Sensing
Date of implementation
Launched 8 April, 2010
Organisation responsible
European Space Agency (ESA)
Purpose
To measure the thickness and monitor the changes in polar ice (sea ice and ice sheets).
Aims
• Measure sea ice thickness and freeboard (height above water). • Monitor changes in Greenland and Antarctic ice sheet elevation. • Determine how polar ice loss contributes to global sea level rise. • Provide long term, accurate datasets to improve climate modelling.
Technology (how it works)
CryoSat 2 uses a specialised radar instrument called SIRAL (SAR Interferometric Radar Altimeter), which: • Sends radar pulses to the ice surface and measures the return signal to calculate surface elevation. Calculates ice thickness by comparing sea ice height to ocean height.
Strengths
• High accuracy • Wide polar coverage: • Specialised for ice • Supports climate science
Limitations
• Cannot measure all ice types equally well • Radar penetration issues • Requires complex processing
Ice loss assessment strategies
• Measuring elevation & thickness • Tracking changes over time • Monitoring glacier edges
Ice loss management capabilities
• Supporting climate models • Informing management