8 Satellite Microwave Radar Observations of Antarctic Sea Ice
181
0
g -5
a)
I!
2 -10
i-IS
E -20
! -25
~ -30
30
40
50
60
70
80
It
0.8
~ ~ 0.6
b)
&~
E 1: 0.4
CD.!
"'"0 0.2
~ e
c~
en
0
30
40
50
60
70
80
-4 c)
-5
-6
m -7
~
i
-8
-9
lH
u
J;
,g -10
• •
• • • . . • •
•
. . •
-11
•
•
•
•
. . •
-12
• •
-13
30
40
50
60
70
80
2.4
c
2.2
~ i 2.0
I!! "0 1.8
"iii 1.6
~:!!. 1.4
f/)
1.2
1.0
30
40
50
60
70
80
Day of Year
Fig. 18. a-d. Time series of a surface air temperatures from the Finnish Salargos buoy; b snow-temperature gradients at thermistor sites on snow-covered perennial ice floes; c 0 or a~yof multiyear
floes (vertical bars indicating range of values), x or aSAR (i.e,. global SAR image means), and. aScatt
or 40· incidence normalized backscatter coefficient; d • EScat backscatter gradient M (linear
regressed) at 40° incidence. For further details, see text (after Drinkwater and Lytle 1997).
Précédent

- 186/292

Suivant