International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences, Vol XXXV, Part B4. Istanbul 2004
‚Choose study area
Synchronous
. monitoring —
| | radiometric correction |
Y
— Geometric correction |
“Image data
pretreatment
| | atmospheric correction |
|
| Empirical regression - |
Construct | | model
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Analysis of =
results
Figure l. The Frame of Research Plan
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2. DATA COLLECTION AND PROCESSING
2.1 Synchronous Monitoring
Water quality monitoring experiment synchronized with
Landsat satellite was performed in PoYang Lake in July 8, 2001.
The locations of sampling points were set as Figure 2.
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Figure 2. Distribution of sampling points
There were ten sampling points, at which SS, chl-a, TN, TP,
CODmn, DO, temperature and pH were monitored. DO,
temperature and pH were measured in situ, and the others in
laboratory. Data of longitude and latitude were obtained by
GPS at each point in situ.
2.2 Remote Sensing Data
Remote sensing data adopted synchronous Landsat 7 ETM+
data for its good spatial resolution, which path/row numbers
were 121/40. The satellite image was clear and cloud-free.
2.2.1 Pre-processing of Remote Sensing Data
The remote sensing data needs several steps of pre-processing
before an inversing model is applied, which include radiometric
correction, geometric correction and atmospheric correction.
Commonly the purchased image has been processed by
radiometric correction and original geometric correction, so
jobs that users need to do are accurate geometric correction and
atmospheric correction. The accurate geometric correction in
this study was accomplished by ground control points (GCPs),
678
whose precision was better than one pixel. The following part
discussed the procedure of atmospheric correction.
2.2.2 Atmospheric Correction
PCI, a commercial image processing software package,
provides a set of atmospheric correction tools for sensors of TM,
MSS and SPOT, such as ATCORO, ATCORI and ATCOR2.
The flow chart of atmospheric correction is showed as Figure 3.
Original Data: TM/MSS or SPOT3/4
*
ATCORO Define aerosol optical depth: VISIBILITY |
: x. :
. Create reflectance image:
cATCOR | Using ATCORO to give VISIBILITY.
Y
Reflectance Image Without Adjacency Effect
FAV Lowpass filter
En Create lowpass reflectance image
Y
Lowpass Reflectance Image
ATCOR2 C reate improved reflectance image with
.adjacency effect — ——
Y
Reflectance Image With Adjacency Effect
Flow chart of atmospheric correction provided by
PCI
Figure 3.
The theory of this method is given by Richter (Richter, 1990;
Richter, 1996), whose main idea is that according to standard
atmospheric categories, atmospheric dispersion has been
calculated in different aerosol types, different sun zenith angles,
different altitudes and different atmospheric visibilities, the
results of which are stored in a directory, like as look-up table.
In actual application atmospheric correction is performed
according to this table. Categorizing basis of Richter method
comes from middle resolution atmospheric transmission model
- MODTRAN. Its arithmetic also considers and corrects the
adjacent effect of ground reflection.
3. EMPIRICAL REGRESSION MODEL
Empirical Regression Model often sets remote sensing data
(atmospheric correction or not) as independent variables and
concentration of water quality components as dependent
variable(s) to construct their relative equations. In order to
review effects of empirical regression models, this study
designed following combinations, and detailed description was
showed in the previous study (Kuang, 2002) .
€ Atmospheric correction: yes or no. two cases.
€ Independent variables: 89 kinds of remote sensing band
combination, such as RI, RI*R3, (R3*R5)/In(R1*R2)
and so on (Kuang, 2002).
€ Dependent variables: SS and chl-a.
3.1 Results of Regression Model
The datasheet of water quality monitoring and remote sensing
data were showed in Table 2. Calculating the relative
coefficient of every above combination (the total mounts of
combination were 356), results that had good correlation were
listed in Table |.
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