Full text: XVIIIth Congress (Part B7)

ALING 
nany 
ly for urban 
ses force to 
nt there is a 
. The entire 
ISive. This is 
ich maps for 
rks out the 
) calculate a 
to separate 
A threshold 
arly-morning 
set contains 
lights (noon, 
ng, and the 
oden, Flora, 
e stádtische 
mittel- und 
der Qualität 
finanzierbar 
adalus-ATM- 
ier erläutert. 
ahr sensibel 
versiegelter 
nwertes ein 
fliegung auf 
ns wird eine 
Kanálen, die 
daraus eine 
tablish more 
ven unsed 
ecessary, 10 
ise existing 
have survey 
of sealing i^ 
arters a map 
ore detailed 
planning a scale of 1: 5 000 is needed. These maps can be 
produced by innovative and efficient methods using 
remotely sensed data. 
The presented investigations are part of a project financed 
and supported by the "Saxonian Department 
environment and Geology" (LUG, Q2500/9) and co-ordina- 
ted by the "Environmental Research Centre Leipzig-Halle 
(UFZ)'. 
2. DATA ACQUISITION 
91 Flight Mission 
The following investigations are based on a flight mission 
over parts of the City of Dresden, Germany. 
The chosen flight areas cover 40 test sites (145,3 ha) 
where a terrestrial investigation of soil sealing was 
undertaken by collaborators of the Institute of Ecological 
Spatial Development (Heber, 1993) over the last years. 
Most of typical surface cover materials in urban 
agglomerations are also recorded in the flight area. 
  
  
  
  
  
  
  
  
  
  
  
  
  
Flight Area |Flight Area |Flight Area 
West (1) Centre (2) |East (3) 
Length in m 4 200 9 000 5 800 
Scan rows 4 000 8 000 5 100 
Width in m 2 200 2 700 2 700 
Number of flight stripes 3 4 4 
Total area in km? 19,9 23,5 18,0 
Flight path direction WNW-ESE |SSW-NNE |NW-SE 
Number of covered test sites |9 17 14 
Total area of test sites in ha — |28,3 84,3 32,8 
  
  
Table 1: Geometric Parameters of the Three Flight Areas 
The flight mission was performed by the "Department of 
Optoelectronics" of the "German Aerospace Research 
Establishment (DLR)". The aircraft was equipped with a 
DAEDALUS-ATM-Scanner AADS 1268. With a flight 
altitude of 500 meters the resolution was 2,5 mrad IFOV 
(Instantaneous Field of View) and flight paths had a lateral 
  
overlap of 40 %. 
In total four flights were carried out, one flight at high noon, 
Wo fights after dusk and one flight before dawn. Table 2 
Shows it in detail: 
for 
487 
  
  
  
  
  
  
  
  
  
  
Date Time Comments 
10.08.95 |12.40 - 13.43 |Multispectral data (12 bands) and, 
additionally, taking of CIR aerial photos 
10.08.95 |21.08 - 22.14 |Only thermal infrared data (band 11), not 
processed yet as the morning flight was 
broken off (technical problems) 
11.08.95 |20.59 - 22.07 |Thermal infrared after dusk 
12.08.95 |04.16 - 05.22 |Thermal infrared before dawn 
Table 2: Program of the Scanner Flight Mission 10.-12.08.1995 for 
Dresden, Germany 
During the evening and morning flights only data from 
thermal infrared bands were recorded, as there were all 
bands registered during day time. 
Band 12 is spectrally similar to band 11, but because band 
11 was partly overmodulated, the intensification of band 12 
was reduced. Simultaneously to scanner recording, CIR 
photos were taken by a specific camera called Zeiss 
ReihenmeBkammer (RMK) 415/23 (calibrated focal 
constant = 153 mm), which was equipped with a KODAK 
Aerochrome Infrared 2443 film. A Zeiss filtertype D 
(Diaphragm 5,6; exposure 1/200) was used. The photo 
scale was 1 : 3 000, the forward overlap was 60 95, and the 
side overlap was 40 96. 
The weather conditions during flight time were extremly 
fine, no clouds and little humidity. Parallel to the airborne 
measurements the meteorological parameters temperature, 
steam pressure, wind direction, and wind speed were 
recorded on two fixed locations. Along three parcours in the 
overflown area temperature and steam pressure were also 
recorded. 
2.2 Quality of Scanner Data 
Because of good recording conditions and long-time 
experience of the "DLR"- colleagues the quality of received 
data is excellent. The geometric resolution of digital 
scanner data is 1,1 m. Only eight lines were not recorded. 
During the noon flight the air temperature was very high 
(about 26 °C), so that surface temperatures in thermal 
infrared band 11 sometimes increased over the blackbody 
temperature of 48,5 °C. This increase could partly be 
avoided in band 12 by reducing the intensification. In this 
band there are also some overmodulations contained with 
the typical shade effect of 2 pixels. The remission of metal 
and glass roofs gives wrong temperature information, 
because the degree of emission £ is less than 0,98 (£ 
0,01 - 0,05; € goss! 0,94) which is assumed as standard. 
metal * 
The flight parameters were stable because of good wind 
conditions, so there was little roll, crob, and pitch distortion. 
This condition was very helpful to find the ground control 
points to rectify data. 
The days of flight mission followed a long, dry period with 
high temperatures, so especially short-cut grass was 
International Archives of Photogrammetry and Remote Sensing. Vol. XXXI, Part B7. Vienna 1996 
 
	        
Waiting...

Note to user

Dear user,

In response to current developments in the web technology used by the Goobi viewer, the software no longer supports your browser.

Please use one of the following browsers to display this page correctly.

Thank you.