The NASA algorithm by [Gloersen and Cavalieri, 1986] is a further development of an earlier version of the same algorithm [Cavalieri and Gloersen, 1984]. It uses the satellite data to calculate two ratios: the polarization ratio (PR) and the spectral gradient ratio (GR):
where ,
and
are the brightness
temperatures in the 37V, 19V and 19H channels, respectively. These ratios are
supposed to be largely independent of physical temperature [Cavalieri
and Gloersen, 1984]. A typical PR-GR plot is shown in Figure
1.
Figure 1 The geometry of NASA algorithm (from [Gloersen
and Cavalieri, 1986])
Tim Flintholm Fink<tff@emi.dtu.dk>