How Radar Altimetry Works: Microwave pulses emit from the satellite antenna toward the ocean. The round-trip pulse travel time τ = 2h / c measures distance to the surface down to millimeters. The shape (slope) of the returning waveform reveals sea roughness (Significant Wave Height), while the amplitude indicates wind speed.
Geostrophic Current Balance: Water mounds up over warm ocean eddies. Earth's Coriolis force balances these pressure gradients, creating geostrophic currents: u_g = -(g/f) · (∂η/∂y).
NASA Oceanography Doesn't Stop at Earth: The same radar altimetry and ice-penetrating radar techniques pioneer ocean exploration across the Solar System!
Europa Clipper (REASON Radar)
Uses dual-frequency ice-penetrating radar (9 MHz and 60 MHz) to sound through Europa's 15-25 km ice shell, searching for subsurface salty water pockets and the global ocean beneath.
Cassini & Dragon (Titan Seas)
Cassini radar altimetry bounced pulses off Titan's liquid methane/ethane seas (Kraken Mare & Ligeia Mare), measuring sea bathymetric depths down to 160 meters.