S, Vol. XXXVIII, Part 7B
In: Wagner W„ Szekely, B. (eds.): ISPRS TC VII Symposium - 100 Years ISPRS, Vienna, Austria, July 5-7, 2010, IAPRS, Vol. XXXVIII, Part 7B
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In the following sections the methodological generic approach
implemented on LCS is described, with specific emphasis on
the critical subsystems. Moreover, a prototype application of
LCS being implemented in the framework of the European
Space Agency (ESA) Support by Pre-classification to specific
Applications (SPA) is described; finally the preliminary results
obtained during the SPA Project are discussed, with the clear
aim of demonstrating the validity of the approach.
1.1 Related work
Many approaches and methodologies exist for land cover
change analysis: an extensive survey is provided in (Lu et al.,
2004). Similar work for multi temporal analysis systems has
been performed to provide targeted land cover change studies or
develop databases of land cover (Homer et al., 2004). An
interesting bi-temporal approach to land cover change analysis
is provided by the Land and Ecosystem Accounting (LEAC)
methodology whose main goal is to provide an easy and
comprehensive access to land cover data, showing the ‘stock’
available for each land cover class in the different land cover
data, and providing also the changes occurred in the periods
between different land cover works, as land cover flows matrix
(Haines-Young and Weber, 2006). The LCS approach however
is not focused on a particular change pattern, land use typology
or phenomena, it is instead proposed a generalized approach to
land cover change analysis that, building on top of land cover
maps stock, might serve as an interactive framework and tool
for scientists to help quickly verify hypothesis and improve
their research activities. Lastly, the system targets also decision
makers to provide a practical surveying tool to systematically
provide fast response in detection of features of interests.
2. METHODOLOGY
The LCS system is a generic tool for long-term time series of
satellite data management for application in the LULCC field.
The term “generic” refers to the wide applicability of the
system to different type of satellite-borne sensor data,
permitting also multi-sensor applications, and to different time
frames; moreover it refers to its ability to fully exploit the
multitemporal database for different LULCC phenomena
analysis.
LCS creates time series of homogeneous satellite data making
use of a robust land cover classification system named SOIL
MAPPER®: this system process satellite data coming from
different sensors in the same way, generating land cover
classification maps with the same semantic meaning, thus
permitting multi-temporal and multi-sensor applications.
The stock of classification maps, are then mapped on a common
reference grid to allow worldwide pixel based multi temporal
analysis of land cover to be performed in relatively small
amounts of time since data compression, obtained through
semantic feature extraction, delivers a map stock within 6
Terabytes, that is an amount of data readily manageable by
modern computer systems.
The core change detection feature of LCS are the land cover
evolution models and its model matching engine: in LCS, an
evolution model is defined as a sequence of expected land cover
classes along the temporal line; each land cover class -
temporal reference pair constitutes an evolution model element.
Land cover transitions can be represented by pairing elements
which define expected land cover configuration in given points
of the time line. A series of evolution model elements defines a
land cover evolution pattern that can be matched with actual
land cover time series data to determine if that data matches the
modelled evolution pattern.
There is almost no automation in model definition and the
model itself is designed to let the user precisely define each
model element, also starting by a derived model from observer
data, with tolerance margins in both feature and time domains.
All the knowledge for multi temporal analysis is provided by
domain experts in the form of evolution models.
The LCS methodology, explained hereafter in its critical
subsystems, foresees three main elements that, chained
together, aim at providing a consistent system for multi
temporal land cover data analysis: original data classification,
Earth fixed reference system and land cover evolution
modelling and matching. Moreover the layout of user interfaces
suitable to ease analysis, define evolution models and perform
automated model matching are described. Following
subsections detail each main aspect of this methodology.
2.1 Common land cover classification system
SOIL MAPPER® is a fully automatic software that permits to
generate land cover classification maps through the analysis of
multispectral satellite data in the optical domain.
As input it requires multispectral remotely sensed (RS) images
calibrated on Top of Atmosphere (TOA) physical values: TOA
Reflectance values for Visible (VIS), Near Infrared (NIR),
Short Wave Infrared (SWIR), Mid-Wave Infrared (MIR) bands
and brightness temperature (BT) for Thermal Infrared (TIR)
bands (Mantovani et al. 2009).
As output, it generates a preliminary classification map where
each pixel is associated with one label belonging to a discrete
set of spectral categories. Spectral classes detected by SOIL
MAPPER® have a semantic meaning belonging to the following
main categories: Vegetation, Bare soil / Built-up, Snow / Ice,
Clouds / Smoke plumes, Water / Shadows, Outliers.
SOIL MAPPER® actually supports most common satellite
optical sensors (from medium to very high resolution), like:
MODIS, AVHRR, AATSR, MERIS, Landsat 5 TM/7 ETM+,
ASTER, SPOT-4 HRVIR, SPOT-5 HRG, IRS 1-C/-D, IRS-P6,
IKONOS, ALOS/AVNIR-2, QuickBird.
Recent developments to the system (MEEO, 2010) introduced
an uniform classification output with similar number of
semantic classes across sensors and standardised classification
output that makes is suitable for LCS.
2.2 Earth Fixed Grid reference
LCS defines a multi level global Earth fixed reference on which
all satellite data has to be remapped to perform multi-temporal
sample-by-sample analysis. The multi-level mesh-grid has been
set with a variab'e uniform angle sampling rate over the
geographic coordinates system (Lat. Lon.) with level 0 set at
1/256 th degree. Samples (grid elements) are grouped together in
fixed size tiles of 64 by 64 samples called Tiles. At level 0 each
Tile covers *4 of degree in both Latitude and Longitude; each
further level doubles the sampling rate in both dimensions (i.e.
1/512 th degree at level 1 and so on). According to (Sahr et al.,
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