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2. EXPERIMENTAL DESIGN
2.1. The Walnut Gulch 92 (WG' 92) experiment:
To investigate the use of combined optical-microwave remote sensing, an experiment was conducted during the
1992 dry and monsoon (wet) seasons in the USDA-ARS Walnut Gulch experimental watershed (southeastern
Arizona). Rainfall typically ranges from 250 to 500 mm/year in this region with almost 2/3 occuring during the
summer "Monsoon" season in July and August. Nine Landsat TM scenes, three SPOT HRV scenes and five
ERS-1 SAR images were acquired to monitor the seasonal surface changes. Eight subsites (METFLUX 1 to 8)
were selected within the watershed to assess the spatial variability of vegetation, soil and meteorological
properties, with a particular monitoring of METFLUX 1 (Lucky Hills) and 5 (Kendall). For each of the
METFLUX (MF) sites, a 5x3 TM pixels target (150x90 m) was defined and used for ground based spectral
measurements as well as for vegetation and soil measurements. The vegetation is basically composed of grass
and bushes in variable proportions as shown in the table below:
sites
dry
biomass
(g/m2)
% shrub
biomass
litter
(g/m2)
vegetation
cover
(%)
rock surface
cover
(%)
MF1
228.7
99
96.8
28
46
MF2
289.9
72
94.8
51
48
MF3
228.0
89
32.3
42
45
MF4
224.8
24
48.6
62
59
MF5
102.3
33
57.4
44
54
MF6
458.6
92
57.1
38
52
MF7
140.2
67
155.2
32
10
MF8
1033.0
99
95.8
40
58
Table 1: mean surface characteristics of the eight metflux sites
Systematic gravimetric surface soil moisture samples (0-5 cm) were collected throughout the
monsoon season at four representative metflux sites (1,3,5,6) with some additional sites depending on satellite
overpasses and continuous TDR and tensiometric cubes measurements at Kendall and Lucky Hills. Volumetric
soil moisture were then deduced from bulk density measurements. This volumetric soil moisture will be later
expressed in percent soil moisture (% sm).
2.2. ERS-1 images
Five ERS-1 scenes were obtained during the experiment around 18h00 UT (llhOO local): days of year (DOY)
135, 170, 240, 275, 310 (35 days repeat orbit) covering only a west part of the watershed (MF 1,2,3,7,8). The
characteristics of this spacebome Synthetic Aperture Radar (SAR) are 5.3 GHz (C band), W polarization, 23°
incidence and 2.5 dB radiometric resolution at -18 dB. We used the standard PRI products provided by the
European Space Agency (ESA) that is amplitude images processed as 3-looks (reduced noise) ground range
(equal size pixels of 12.5x12.5 m) calibrated digital images.
The images were georeferenced using 1:5000 scale orthophotos of the US Department of
Agriculture-Agricultural Research Service. Because of the speckle effect, it was sometimes difficult to define
enough ground control points, or to locate them, to perform accurate geometrical rectification. However final
transformation RMS error was around 2 pixels (i.e. 25 m) which was quite satisfactory to locate the MF targets.
A multitemporal SAR image has thus been produced, showing contrasted pattern in terms of dry to wet
conditions evolution. Backscattering coefficients o° were then extracted on each of the images for all the
150x90m targets using the formulation below:
a°(dB) = 10 log <DN 2 > -K + p (1)
P= 10 log Sm (2)
sm a nf