S, Vol. XXXVIII, Part 7B
In: Wagner W., Székely, B. (eds.): ISPRS TC VII Symposium - 100 Years ISPRS, Vienna, Austria, July 5-7, 2010, IAPRS, Yol. XXXVIII, Part 7B
73
They remain on a level
crease in October. In
alues for maize fields
July. Tobacco, which is
n April to July to a high
g this peak, it turns to
until harvest in October,
for broad-leaved crops
ed to the one of HH
the results for Fuhrberg.
is comparable to the one
iach such high values,
gh backscatter values in
¡ignificantly lower. HH
vide range from April to
most values decrease to
for wheat and rye. After
:mber and than decrease
grain crops in Fuhrberg
bin a wider range. An
i observed likewise, but
lore, there is an explicit
ns with wide distributed
lg in Fuhrberg. There is
I backscatter during the
intly lower. In June and
'alues can be found. In
3 for rye and 3.2 dB for
;es from 4.1 dB for rye
ase is less with mean
i (oat). VV backscatter
anger than for grains in
ickscatter for grasslands
of <-10 dB. The only
i with clearly higher
irement in June with -
ch values as low as the
t relatively low value
e Gorajec region. An
» the one in Fuhrberg,
Fuhrberg is observable
hen grain crops or bare
lower during all month
month the decrease is
^arable to the Fuhrberg
ind meadows.
4S
for the different crops
backscattering patterns
y using time series of
e all over the year
ons, the phenological
r can be detected. This
of broad-leaved crops
¡crimination within the
beets and maize). The
fill has some problems,
to its very specific
s can be differentiated
given for applications
is often not available
The high resolution of the radar images allow for a fine grained
description of the inhomogeneities of the soil and/or plant
structure. This is clearly visible from the different results of the
German and Polish fields. These differences can be explained
with the highly diverse conditions in both study areas (higher
weed content, lower agricultural production standard,
undulating terrain with resulting differences in local incidence
angles for the radar signal, and smaller fields in Poland). This
can be a disadvantage because it results in additional scatterers
distorting the crop reflection. On the other hand, it might be
used to derive e.g. the weed content if fields with the same crop
are compared. Further investigations are necessary to come to
conclusions.
These first results about the characteristic backscatter properties
for different crop types which are comparable for both research
areas already show the high potential for multi-temporal land-
use classification with high resolution, satellite based synthetic
aperture radar. Especially, the possibilities for detecting the
different crop types provide a first important precondition for
the derivation of soil erosion risk: crops with a high risk for
erosion can be separated from those with a lower risk. This
information can be mapped for the respective regions and
provides input data for the C factor, an important parameter for
the calculation of soil erosion with the Universal Soil Loss
Equation (USLE). The provision of exact information about
crops and their phonological development during the year is a
central issue for the quality of erosion risk calculation
(Meusburger et al., 2010).
The high resolution of the radar data allows also for the
detection of smaller structures like hedgerows and field
margins. It will be the next step to collect respective ground
truth to compare the backscatter values of these biotope
structures.
Further on, enhanced classification approaches have to be tested
which make use of the information from the time series and the
polarisations to derive the best classification results. An extent
of the developed classification method on more subtle habitat
structures within agricultural areas, e.g. woody landscape
elements or field margin strips, will follow. Afterwards the
suitability of the classification results for the assessment of
biodiversity and soil erosion changes will be evaluated. Thus
effects of land use and its changes on the selected ecosystem
services will be elaborated.
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