Phone: +64 7 8384466,
Fax: +64 7 8384633
Email: larsb@waikato.ac.nz
Terrain features at a multiple of scales affect soil properties, drainage, climate and ultimately species habitat. For example, macro scale terrain features, such as the large open valleys of the eastern Southern Alps, create wind tunnels and are subject to large mass movements and erosion deposits. Meso and micro scale valleys may provide a more sheltered environment from winds but be subjected to more frequent frosts. It is important therefore to identify a range of terrain features that vary in scale if terrain is used for species habitat modelling.
Rather than identify a large range of possible terrain features and work with a nominal terrain classification, it is more practical for biodiversity mapping to work with terrain indices that take into consideration the important habitat properties of different terrain features. Important habitat properties of a terrain feature are whether it is subjected to erosion attrition or erosion deposits, has good or poor water drainage, and is sheltered or exposed to climate. If terrain indices are able to differentiate these important micro climate and soil properties, then terrain indices could be used as surrogates of these properties.
One such index can be obtained by subtracting the mean elevation from the
actual elevation. The mean elevation is calculated by using a focal neighbourhood
function. This index indicates whether a location is above the surrounding
terrain (like a ridge) or below the surrounding terrain (like a valley floor)
or somewhere in between. By varying the extent of the neighbourhood when
calculating the mean it is possible develop a series of indices that identify
terrain properties at different scales. Figures 1 -3 shows three terrain
indices that distinguish terrain properties at three different scales. These
figures show 3D perspective views with the vertical dimension being the
actual elevation and the relative values of the terrain indices draped over
the elevation using a continuous grey scale. It is therefore possible to
compare the terrain indices with the actual terrain surfaces. Figure 1 shows
a terrain index based on a 10 km neighbourhood radius for a section of the
Wilberforce Valley (viewed from near Lake Coleridge). It can be seen that
it distinguishes the large valley floors from the mountain ranges. Figure
2 shows a terrain index based on a 1km-neighbourhood radius for Mt Karioi
(viewed from the South West). As you can see, it distinguishes the gullies
from the main ridges and spurs. Figure 3 shows the same view of Mt Karioi,
but displays a terrain index based on a 100m neighbourhood radius. This
distinguishes small indentations on the side of spurs and ridges. These
terrain indices could be used as surrogates for micro climate and soil properties.
Figure 1 Section of
the Wilberforce valley showing a Terrain Index based on a 10km Neighbourhood
(Cellsize 500, Continuous grey scale from
-829 to 1124. Light is low and dark is high. The mean value is -13)
Figure
2 Mt Karioi showing a Terrain Index based on a1km Neighbourhood
(Cellsize
50m.Contiunous grey scale from -115 to 190. Light is low and dark is high.
The mean value is -3)
Figure 3 Mt Karioi
showing a Terrain Index based on a 100m Neighbourhood (Cellsize 50m. Continuous grey scale from
-34 to 61. Light is low and dark is high. The mean value is -3) Once species location information has been integrated with environmental
character data, such as in Table 1, it is then possible to export the table
into statistical software and do complex multivariate analysis (this research
is still in progress). It is also possible to use GIS to graphically represent
the data as described in the next section. Figure 4 shows an example of the visualisation
functions of a GIS using the species Tawa. This information was extracted
from a 20,000 record data set that was derived from integrating a subset
of the NVS data bank with environmental character data. The resulting graphic
contains both presence and absence information and uses a combination of
maps, graphs and univariate statistics. This graphic takes approximately
10 minutes to produce and could be completed for all the species recorded
in the data set. Currently there are only 33 species in this relational
data set. Visualisations of other species
can also be viewed.
The graphical display of environmental characteristics of the habitat of
a species helps people understand the complex nature of species distribution
patterns. It perhaps raises more questions than are answered but the technique
is very useful for encouraging further research and analysis. The graphic
displayed in Figure 4 could be improved with
the inclusion of multivariate statistics, a predicted distribution map,
and statistical error information. It is conceivable that if species distribution
data were made available in a relational format, it would be possible to
produce graphics for every species. These graphics could be compiled into
a publication on the Internet that was updated as new data distribution
information was received. Such a publication could be used to ascertain
priority areas for future data collection and analysis.
2.2 Data Integration
There is now a range of GIS data sets that can be used to derive environmental
characteristics of each plot. These include the terrain indices previously
described, a range of climate parameters (such as minimum and maximum temperatures,
rainfall, and solar radiation), geology, distance from coast, and the main
landcover type. It is a relatively simple and routine operation to integrate
geographically referenced databases, based on a common location. The NVS data
set contains the NZMG co-ordinates of each plot, so it is therefore possible
to identify a range of environmental characteristics of each plot location
and combine this information to the NVS data set. Table 1 illustrates this
concept. It shows a sample of information obtained from NVS, with 19 records
of known locations of Fushica execelsar expressed as NZMG co-ordinates
(Eastings and Northings). GIS, in combination with a range of environmental
data sets, was used to derive environmental characteristics of each known
location. This data integration can be implemented for large data sets containing
20,000 records within a few minutes.
2.3 Data Visualisation
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Table 1: Data Integration
In 1999, Landcare Research priced the cost of transfer of the NVS data
bank at $3110 and the format would be as individual plot files. The Herbarium
Specimen database was priced at $11,109. These two data sets are very important
biodiversity data sets. Even though the collection of the data in these
data sets have been a substantial investment of state funding and the conversion
of this data to a digital format has used additional state funding, they
are not easily accessible to researchers. Not only are these data sets
expensive to obtain they are also in an unfriendly individual plot file
format, rather than a relational table format that can be easily used by
standard database software. Landcare Research charged $1300 for a copy
of the Land Resource Inventory and $700 for the climate data. Not only
were there charges for the transfer of data, but signed contracts were
required implying that Landcare Research has copyright on this "Public
Good" data. This contract understandably includes a disclaimer but also
prevents the sharing of data and is restrictive on use. On a more positive
note, Landcare Research provided a subset of the NVS data bank for free
which was in a user friendly relational format, and the Institute of Geological
and Nuclear Sciences provided a Geology GIS layer for free. It is this
more collaborative, "Public Good" approach that will lead to the development
of biodiversity analysis tools and a more informed and educated public.
Biodiversity is a "Public Good", therefore any agent, whether publicly
or commercially funded, that improves biodiversity information and its
dissemination is providing a "Public Good". These agents, whether public
or private, should be encouraged and assisted to use the best biodiversity
data available.
Given that GIS requires coordination and calibration at a strategic management level, it is important that high level managers also have a general understanding of GIS functionality and application. Although it can not be expected that strategic managers be capable of using GIS, they need to be aware of its functionality and the issues relating to its implementation. There is a need for coordination of environmental information collection and dissemination.
With the appropriate databases made accessible in New Zealand and with
the functionality of GIS analysis, the development of useful biodiversity
and species habitat distribution models are possible. Such initiatives
need to be instigated by independent research teams that can validate and
critique each other's work to ensure such models are of scientific quality.
The independent validation of research requires data to be shared and results
and findings to be made known. Without such a process, there is no science.
Francis,
H. D. 1985 Soil landscape analysis, London : Routledge & Kegan Paul.
Gahegan, M., 1999 Four barriers to the development
of effective exploratory visualisation tools for the geosciences. Int.
Jrnl. Geographical Information Science 13(4): 289-309.
Geiger,
R. 1971 The climate near the ground. Harvard University Press, Cambridge.
Lehmann, A., Leathwick, J. and Overton, J. 2000 Assessing
hotspots of New Zealand fern diversity using Generalized Regression Analysis
and Spatial Prediction (GRASP) 4th International Conference on Integrating
GIS and Environmental Modeling (GIS/EM4. Banff, Alberta, Canada, September
2 - 8, 2000.
Stafford,
S.G., J.W. Brunt and W.K. Michener, 1994: Integration of scientific information
management and environmental research. In: Michener, W.K., J.W. Brunt and
S.G. Stafford (editors), Environmental Information Management and Analysis.
Taylor and Francis, Bristol.
Tivy, J. 1993 Biogeography - A study of plants in
the ecosphere. Longman, Harlow.