High-density geostationary satellite wind observations have become an impor
tant new contributor to the observing network over oceanic regions. During
the 1998 North Pacific Experiment (NORPEX), assimilation of these data in t
he Navy Operational Global Atmospheric Prediction System (NOGAPS) provided
substantial improvements in 48-h forecast skill over the northeast Pacific
and western North America. The current study shows that the large positive
impact of the geostationary satellite winds results mainly from the reducti
on of analysis errors that project onto the leading singular vectors derive
d from the linearized forecast model. These errors account for only a small
fraction of the total analysis error and, during NORPEX, were confined mos
tly to the middle and lower troposphere with maxima over the central Pacifi
c. These errors do not necessarily coincide with the locations of the large
st analysis errors. Experiments in which the satellite information is retai
ned only at prescribed vertical levels in the analysis confirm that the inc
rements in the middle and lower troposphere account for most of the forecas
t impact.
Implications for the design of future observing systems, including strategi
es for targeted observing, are discussed. It is argued that the results sup
port the key underlying principles of targeted observing, namely, that the
early stages of error growth in most numerical weather forecasts are domina
ted by a relatively small number of unstable structures, and that preferent
ially reducing analysis errors that project onto these structures can produ
ce significant improvements in forecast skill.