Imbers
' OCTS
ge wil
ally for
during
\, three
roduce
OCTS
nages)
ny pixel
GLI are
nposite
itoring,
th the
ing the
ALI for
thod of
L| data
in this
| using
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ud free
ems on
urnal of
e effect
ensing,
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34-41.
Table1 Characteristics of satellite /sensors
NOAA-9 / AVHRR NOAA-11/AVHRR ADEOS/OCTS ADEOS —II/ GLI
"height (km) 850 850 797 802.9
period (min.) 102 102 101 101
inclination (deg.) 99 99 98.5 98.62
FOV (deg.) [swath] +55.4 [3,000 km] +55.4 [3,000 km] +40 [1,400 km] +45 [1,600 km]
IFOV (mrad) 0.944 [1.1km] 0.944 [1.1km] 0.85 [750m] 1.258, 0.3125
[spatial resolution] [ 1km, 250m]
recurrency 7 = 14 +1/8* = 14-179? 14 + 11/41 14+1/4
lines per one scan 1 1 10 12
local time at approx. 2:20*) approx. 1:40?) 10:30 +15 10:30 +15
descending node
spectral bands vis - near IR (2) vis - near IR (2) vis - near IR (8) vis - near IR (22)
thermal IR (3) thermal IR (3) thermal IR (4) short IR (5)
thermal IR (7)
*) The angular velocity of NOAA satellite is delayecd gradually. Consequently,
the recurrency becomes less and the local time at descending node becomes later.
Figure 1
AVHRR 3 deg
date +3 +2 +1 N -2 -3
Q A o a Q. Q
x 7 aJ
30de
5
e
WV» 1
e
8.8 deg uh
OCTS
-]
10 12 7 4 -$ +15 +4 181 +12. s 4
date e Ges hi FS tuo al N ARNO + -14 +16
DO OR RR A RD OO OH AD ln On
eA
797 m
LENS ANN, ANY
Lo INS NAN
4 + KA Jo] 5e
NS NA, OÔLS deg
ON NN NE
date 71
802.9 km
8.5 deg
Consecutive orbit positioins and observed coverages (on the equator)
279
International Archives of Photogrammetry and Remote Sensing. Vol. XXXI, Part B7. Vienna 1996