C. Mejia et al., DETERMINATION OF THE GEOPHYSICAL MODEL FUNCTION OF THE ERS-1 SCATTEROMETER BY THE USE OF NEURAL NETWORKS, J GEO RES-O, 103(C6), 1998, pp. 12853-12868
We present a geophysical model function (GMF) for the ERS-1 scatterome
ter computed by the use of neural networks. The neural networks GMF (N
N GMF) is calibrated with ERS-1 scatterometer sigma 0 collocated with
European Center for Medium-Range Weather Forecasts (ECMWF) analyzed wi
nd vectors. Four different NN GMFs have been computed: one for each an
tenna and an average NN GMF. These NN GMFs do not present any signific
ant differences which means that the three antenna are quasi-identical
. The NN GMFs exhibit a biharmonic dependence on the wind azimuth with
a small upwind-downwind modulation as found on previous GMFs. In orde
r to check the validity of the NN GMF systematic comparisons with the
European Space Agency (ESA) C band model (CMOD4) GMF (version 2 of Mar
ch 25, 1993) and the Institut Francais de Recherche pour 1'Exploitatio
n de la Mer (IFREMER) CMOD2 I3 GMF are done. It is found that the NN G
MFs are highly accurate and relevant functions to model the ERS-1 scat
terometer sigma 0.