Full text: XVIIIth Congress (Part B1)

  
  
-80t 
North(km) -relative to the base receiver 
o 
o 
  
  
  
= + 
mm e 
o 
0 50 100 150 
East(km) -relative to the base receiver 
o 
Figure 2 2D trajectory of the aeroplane, relative to the 
base receiver 
  
  
  
  
  
  
(a) 
2 T 
Bal 
= 0 
5-4 
Zn 2000 4000 6000 8000 10000 
5 (b) 
NE NE des A0 Jo poi 
70 tra iii nié pi einig 
  
  
  
0 2000 4000 6000 8000 10000 
GPS Time (second) 
Figure 3. Real-valued estimates of the cycle slips, 
assuming data gaps of one second. 
(a) 
A 
  
DN 1,-1(cy) 
oN 
1 
N 
  
  
  
  
(b) 
A 
  
N 
  
DN -7,9 (cy) 
M» o 
  
  
à 
  
i i i i 
0 2000 4000 6000 8000 10000 
GPS Time (second) 
Figure 4. Real-valued estimates of the cycle slips, 
assuming data gaps of 60 seconds 
  
  
Latitude error (m) 
  
  
  
  
i i 
0 2000 4000 6000 8000 10000 
  
1 
Le 
o 
  
Longitude error (m) 
o 
  
  
= 
o 
o 
  
i i i 
0 2000 4000 6000 8000 10000 
Cumulative Tracking Time in Seconds j 
Figure 5. Deviations of code DGPS position solutions: 
(a) for the latitude component: o=9.384m; and (b) for 
the longitude component: o= 7.348m 
Filtering (-) and Smoothing (—) Solutions 
  
Latitude error(m) 
N & Qo 
  
  
  
E ————— iX à — — fea 2— —— € 
Q 20 40 60 80 100 
Cumulative Tracking Time in Seconds(1- 1 00) 
  
  
  
  
- 
o 
  
Latitude error(m) 
o 
Oo u = 
  
  
  
  
  
  
  
1 
o 
o 
  
TO 2000 4000 6000 8000 10000 
Cumulative Tracking Time in Seconds(1 00-9300) 
Figure 6. Convergence of the latitude filtering solutions 
with tracking time. Its standard deviation o= 0.255m 
and the bias of smoothing solution: 6 = +0.161m . 
Filtering(-) and Smoothing (--) Solutions 
  
  
  
  
  
  
  
  
  
  
  
  
  
  
— 10 T T 
E : 
A second 
= : 
> -5 Le à 4 A 
-10 1 i i i 
0 20 40 60 80 100 
Cumulative Tracking Time in Seconds(1-1 00) 
p 0 T T T 
E 
E -0.5 
« 
= 
= 1) 
= 
5 
-1.5 
i i i 
0 2000 4000 6000 8000 10000 
Cumulative Tracking Time in Seconds(1 00-9300) 
Figure 7. Convergence of the latitude filtering solutions 
with tracking time. Its standard deviation o— 0.223m. 
and the bias of smoothing solution: ó ^ -0.138m . 
International Archives of Photogrammetry and Remote Sensing. Vol. XXXI, Part B1. Vienna 1996 
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