A new technique is developed for the analysis of satellite data to pro
vide accurate measurements of seasurface temperature (SST). Satellite
data sets are partitioned into subsets depending on the value of a sel
ected parameter (for example, latitude, total water vapor, and water v
apor content of an atmospheric layer) to provide a suite of algorithm
coefficients that reduces the errors associated with the derivation of
SST. For data sets obtained with the along-track scanning radiometer
(ATSR) the data themselves can be used to modify the coefficients used
in the SST algorithm, but for other instruments it may be necessary t
o use additional data sets to select a correct set of algorithm coeffi
cients. A simulated set of ATSR data is used to develop algorithm coef
ficients for different atmospheric conditions, and the improvement in
SST derivation is demonstrated. For ATSR, when all the data for three
infrared channels in both the nadir and forward views are available, t
he improvement is marginal, but for situations when there are limited
data the improvement is considerable. The analysis suggests that in th
e future the best SST analyses will be obtained by developing an inter
active system, where the satellite data are ingested into a numerical
weather forecast model so that algorithms can be selected and applied
with a forecast or analysis of the atmospheric state. The new techniqu
es are tested by application to a large global data set of ATSR bright
ness temperatures. This analysis highlights the future need for large
SST validation data sets that include coincident satellite and surface
-based measurements.