The NOAA series of polar satellites have proved highly useful for stud
ying the ocean surface. In particular, the radiance information obtain
ed through channels 4 and 5 of their Advanced Very High Resolution Rad
iometer (AVHRR), which are sensitive to radiation in the thermal infra
red, allows sea surface temperature (SST) to be mapped with a precisio
n of 0.1-degrees-C. This article describes the way this is done, and h
ow such maps can be processed to study oceanic thermal structures and
their variation. Particular attention is paid to the detection and mon
itoring of the upwelling of cold, nutrient-rich benthic waters from th
e ocean floor, since these areas constitute the richest fisheries.