with limited site data.
The target tree species of this study is Elaeocarpus japonicas
(Japanese Elaeocarpus tree, JET), a kind of evergreen tree
species. It widely spread in whole Taiwan from low upland to
mountainous areas with elevation 2200 m above sea level.
JET is also founded in Japan and China. JET is a kind of
dominant tree species in the Huisun forest station. It is
usually founded on the ridge with thinner soil layer, direct
sunlight and water stress. JET is a kind of pioneer tree species
in second succession, and therefore it plays a necessary role in
ecosystem.
We aimed at applying 3S (GIS, GPS and RS) technology to
derive elevation, slope, aspect and terrain position from DEM
and vegetation index (derived from the two-date SPOT-5
images), and using these five environmental layers to build
predictive models. In this study, we adopted five methods
(DA, DT, MAXENT, ML and DOMAIN) and three sampling
designs (SD) to build “Tong-Feng (SD1)” model, “Kuan-Dau
(SD2)” model and “two watersheds (SD3)”, eventually we
totally built 15 models. The models’ reliability and
performance were evaluated, and used as the criteria of model
comparison.
2. STUDY AREA
We chose the study area with rectangular shape, which covers
the Huisun Forest Station and has the total area of 17,136 ha.
The Huisun Forest Station is in central Taiwan, situated within
242°-24’5" N latitude and 12131217” E longitude. The
station is the property of National Chung-Hsing University, and
study area ranges in elevation from 454 m to 3,419 m, and its
climate is temperate and humid. Hence, the study area has
nourished many different plant species and is a representative
forest in central Taiwan. It comprises five watersheds,
including two larger watersheds, Kuan-Dau at west and
Tong-Feng at east. All of the JET samples were collected
from the two watersheds by using a GPS (Figure 1.).
3. METHODS AND METERIAL
3.1 Data Collection
The collected data contained DEM with 5 m x 5 m resolution,
orthophoto maps with 1: 10,000 scale and two-date SPOT-5
images taken in 2004/07/10 and 2005/11/11. The JET
samples were acquired by field survey with Trimble PRO XR
series GPS system. Furthermore, an expandable antenna rod
with 5m in length and a laser ranging were adopted with GPS
for enhancing the capacity of the system. All of the JET point
data were field-collected from Tong-Feng and Kuan-Dau
watersheds (© SPOT Image Copyright 2004 and 2005, CSRSR
NCU).
5
3.2 Data Processing
Slope and aspect data layers were generated from 5 x 5 m
DEM by using ERDAS Imagine software module. The ridges
and valleys in the study area were used together with DEM to
derive terrain position layer. The main ridges and valleys over
the study area were directly interpreted from the contour lines
shown on the orthophoto base maps; these lines were then
digitized to establish the data layer of main ridges and valleys
by using ARC/INFO software for later use. The data layer of
main ridges and valleys in a vector format was converted into a
new data layer in a raster format by ERDAS Imagine software,
and then combined with DEM to generate terrain position layer
(Skidmore, 1990). The equation is expressed as follows.
Vegetation indices were derived from the two-date SPOT-5
images, one in autumn, the other in summer, by using Spatial
Modeler of ERDAS Imagine. JET samples obtained by a GPS
were corrected by using post-processed differential correction
and converted into ArcView shapefile format for later use.
Pj - PV / (PV 4 PR)
Where PV = the Euclidean distance between a certain pixel P
and the nearest valley pixel;
PR - the Euclidean distance between a certain pixel P and the
nearest ridge pixel;
When Pj = 0.0, it is referred to valley; P; = 1.0, it is referred to
ridge. The P; from 0.0 to 1.0 is partitioned into eight equal
intervals.
The change in water content and pigment composition in plant
owing to the season or stress can be detected by using
multi-date imagery. These two phenomena could result in
changing plant's spectral reflectance of different bands in
multi-band image (Jensen, 2005). The concept of the
vegetation index adopted in this study is explained in Hoffer
(1978). The following equation is used to derive the
vegetation index data layer.
NIB umm = MER ver
NIR — MIR
summer summer
Vegetation Index —
Where NIR summer/autumn iS the reflectance of near infrared band
during summer and autumn, and the reflectance of middle
infrared is denoted as MIR summer/autuma- The output value is
scaled in 8-bits data type.
3.3 Overlaying the Environmental Layers
The layers of elevation, slope, aspect, terrain position,
vegetation index, and JET sample data were overlaid by
ERDAS Imagine software. We used the function “AOI (area
of interest)” in ERDAS imagine software to clip the concurrent
environment factor value of JET locations. These clipped-out
data were used as independent variable for building predictive
model.
3.4 Target and Background Samples
Target sample is the GPS-located JET point sample and the
concurrent environment factor value. The ratio of background
to target we adopted was followed the criteria Sperduto and
Congalton (1996) proposed that the ratio should be more than 3.
The sampling strategy is randomly selected following Pereira
and Itami (1991) suggested avoiding spatial autocorrelation.
3.5 Sampling Designs and Model Building
We designed three sampling designs (SD) for the comparison
of model reliability, “Tong-Feng (SD1)”, “Kuan-Dau (SD2)"
and “merged samples of two watersheds (SD3)”. SDI had
104 individual JET samples, and SD2 had 80. SD3 had all of
the 184 JET samples. For each of these three SDs, the dataset
was split into two subsets, 2/3 and 1/3 of all, used for
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