The ocean surface is scarcely ever absolutely a mirror.  Wind and waves, of course, roughen the surface but this roughness can also be  modified by immersed reefs, oil slicks, small islands or even surface currents.

Altimeters, which basically measure the power backscattered by the sea surface, are very sensitive to the surface roughness, as it modifies the reflection of the radar waves by the sea. The corresponding parameter in altimetry data is called the backscatter coefficient, which  is an average over the altimeter footprint (about 15 km diameter). However, the phenomena listed above are in general of much smaller extent than the footprint and can thus not be detected using the classical (1 second-averaged) data. However, if we consider the high resolution (20 per second) echo waveforms, an altimeter can also be seen as an imager of the sea surface backscatter whose geometry is certainly more complex than the traditional ones, as the pixels are not rectangles but rings. It is thus possible to compute the imaging matrix of the altimeter, which depends only on the orbit characteristics and sensors geometry, and to invert it to retrieve the surface backscatter at a resolution of the order of 300 m.

The Jason-1 and Jason-2 data were thus processed over a small reef, the Erika reef in the South China Sea. This reef, about 2 by 3 km in size, is very shallow (about 2 m depth) and its eastern side can emerged at low tide. Then the emerged area gives a very strong
signature in the altimeter data whilst at high tide the presence of  the reef attenuates the waves and decreases the surface roughness.