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In: Wagner W„ Székely, B. (eds.): ISPRS TC VII Symposium - 100 Years ISPRS, Vienna, Austria, July 5-7, 2010, IAPRS, Vol. XXXVIII, Part 7B
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the area suitable for the cultivation of vines, tobacco (main cul
tivation in the region), fruits and grains. Slopes are deforested
and eroded; with areas prone to landslides. Most of the hills are
covered by low-productivity grassland used for grazing. There
are alluvial and deluvial-meadow soils along the major rivers in
the region, where vegetables and hemp can be grown, due to the
larger quantity of moisture, they receive from the soil layers.
4 REMOTE SENSING IMAGERY
A constellation of 5 multispectral satellite sensors were launched
by RapidEye in August 2008 with a primary focus on agricultural
applications. These satellites have a lifespan of seven years; a
ground sampling distance of 6.5m resampled to 5m; and a daily
overpass. A new feature in RapidEye sensor is the Red Edge band
(690-730nm), which could allow better estimation of the ground
cover and chlorophyll content of the vegetation (Haboudane et al.,
2002, Vinal and Gitelson, 2005). All 5 satellites have the same
calibration coefficients. The radiometric scale factor converting
the image DN values into reflectance is 0.01.
Imagery was obtained from RapidEye AG at standard processing
level 3A 2 (orthorectified) for the dates indicated in Table 1. Pre
processing of imagery was carried out in ERDAS Imagine and
ESRI ArcGIS software. This entailed further geo-referencing of
the satellite imagery to the national orthoimagery provided by the
Bulgarian government, thus ensuring data consistency between
the RapidEye imagery and the LPIS datasets. Nearest neigh
bour approach was used for the resampling. In addition to the
RapidEye imagery, VHR data from IKONOS has been acquired
in the frame of the annual CwRS campaign and was also provided
for the study. The availability of this imagery was an important
source of ground truth. An orthorectification of this VHR data
was carried out using the reference national orthophoto, addi
tional ground control points and the SRTM DEM provided freely.
Acquisition dates in 2009
Zone
April
May
June
July
September
12.04
20.05
10.06
15.07
10.09
KARD
23.07
16.09
24.07
Table 1 : Acquisition dates of all RapidEye images over KARD
5 METHODOLOGY
The proposed methodology is based on the key elements derived
from the GAC definition in Section 2. From the adopted GAC
definition, we can conclude that, a land could be considered in
GAC, if at least the following two criteria are met: i) vegetation
is growing or can be grown on that land; ii) the land is accessible
for agriculture activities (cropping, grazing, etc.). Both criteria
can be evaluated by monitoring the development of the vegeta
tion during the year (phenological cycle), together with the anal
ysis of the texture properties of the land cover and the relevant
spatial context. Thus, the methodological approach was based on
a multi-temporal analysis of RapidEye time-series, using object
oriented classification techniques in order to detect and qualify
the land cover features in respect to their potential to represent
agriculture area in GAC. Considering that the proposed definition
of GAC is quite broad, it was agreed that the first estimation of the
land potentially useful for agriculture (and being in GAC) can be
done through detection and quantification of the non-GAC (and
potential non-GAC) features. From land cover (physiognomic-
structural) point of view, land which is not in GAC is constantly
2 http ://www. rapideye.de/home/products/standard-image-
products/standard-image-products.html
bare or non-vegetated during the (cultivation) year (for example
sealed surfaces; natural bare areas) and contains features prevent
ing the agricultural activity even though it is vegetated (for exam
ple closed forest, woodland, wetland, etc.)
An overview of the proposed methodology used for decision
making and analysis can be seen in Figure 2. The selection, ac
quisition and pre-processing of imagery was important to provide
a solid foundation for future analysis. The acquisition windows
were carefully defined on the base of crop calendars, provided
by ReSAC. Imagery from April, May, June, July and Septem
ber were acquired over the test zones to reflect the phenological
cycles of the vegetation (see Table 1).
Figure 2: Proposed methodology
Data analysis: Capture and qualification of the permanently non-
vegetated areas and the areas not accessible for agriculture were
the primary targets. Most of the non-vegetated area with artifi
cial anthropogenic origin, as urban structures, roads, hardpans,
etc. can be efficiently extracted from a single RapidEye image,
if acquired in the correct period of the year. The same is also
valid for the naturally vegetated areas, not suitable for agricul
ture activities (such as forested areas, wetlands), or water bodies.
However, for most of the natural bare areas, unsuitable for agri
culture (such as as eroded surfaces, degraded soils), the analysis
has to be based on several time series, in order to filter out tem
porary bare areas, for example, harvested agricultural fields. An
other important land cover, requiring multi-temporal approach, is
low-productivity grassland, quite common in the area of KARD.
This type of mountain grassland, used for grazing, appears vege
tated (on the satellite imagery) only during particular periods of
the year (early spring); usually its spectral signature is similar to
bare surface, especially during the summer when it becomes dry.
The only option to efficiently capture those areas is through the
use of multi-temporal imagery covering the entire active agricul
ture period so that various aspects of the vegetation growth and
climatic conditions can be considered.
It was assumed that permanent bare areas should have low NDVI
values in all time series. For that purpose Red Edge Normal
ized Difference Vegetation Index (NDVI) (equation 1) (Wu et al.,
2009) was calculated for all images.
NDVI Red Edge =
NIR — Red Edge
NIR + Red Edge
(1)
The choice of the Red Edge channel, instead of the Red channel
for the NDVI calculation, was mainly driven by lesser saturation
of the Red Edge NDVI comparing to the traditional NDVI over
highly vegetated (forested) regions, as reported in the literature
(Haboudane et al., 2002, Vinal and Gitelson, 2005). Figure 4.b