thern
ellite
oster,
Figure la. F-test parameter, F, for period
lysis t=4yr. F was calculated by applying a
So multiple-window harmonic analysis technique
e to SMMR 37GHz vertically polarized Ty. The
two boundaries define the dry-snow facies and
: the percolation facies according to Benson
1 of (1962).
sing
and
, Pp.
taper
ohys.
8D] < F
ctive
‚ce
is. J. 5174 «Fi «6,51
sive F< 3.74
field
88.
993,
SM/I
site.
ivity
IRR, Fi
51 igure 1b. Absolute value of complex
m: amplitude, [ju], for period c-4yr. |u| was
calculated by applying a multiple-window
harmonic analysis technique to SMMR 37GHz
lite vertically polarized Ty. The two boundaries
ster, define the dry-snow facies and the percolation
facies according to Benson (1962).
onic
rctic
4.5K « Iul
3.0K « Iul « 4.5K
1.5K < lui < 3.0K
lul « 1.5K
747
International Archives of Photogrammetry and Remote Sensing. Vol. XXXI, Part B7. Vienna 1996