Full text: Proceedings, XXth congress (Part 4)

2004 
—— 
land 
:lago 
5-3.5 
1a in 
l00se 
nals. 
iddle 
ality. 
004) 
| Was 
mals, 
nove 
from 
| and 
same 
they 
nter 
e the 
same 
Lures. 
nmer 
laces 
dents 
| the 
area, 
a 
wu. 
n the 
en in 
| they 
nount 
ig the 
d the 
. Ie 
ns in 
er the 
these 
ons. 
noose 
/idual 
rface. 
olitan 
noose 
'egion 
idents 
in the 
International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences, Vol XXXV, Part B4. Istanbul 2004 
  
concentration of moose accidents in connection to the moose 
density has been examined (Häggman, 1999). The density 
surface model played a crucial role also in the definition of the 
ecological network (Väre & Krisp, 2003) and in the application 
for land use planning for the regional plan in Uusimaa (Väre, 
2001). 
2. METHODS - CALCULATING THE MOOSE 
DENSITY 
Using geostatistical methods, available in GIS (Geographic 
Information System) analysis tools, the data can be interpolated 
to density surfaces for the different years. By applying overlay 
and data fusion procedures with road data for the same 
instances, we can highlight changes in moose habitats caused 
by infrastructure. Based on previous research experience we 
decided to use a Kernel estimation method to calculate the 
moose density. Our research area is the area of Uusimaa in 
southern Finland 
2.4 Data 
Finland is divided into 15 game management districts. They 
govern hunting associations, which are usually same size as 
local communes. At Uusimaa district there is over 30 
associations, which are furthermore divided to over 300 hunting 
clubs or parties. The data about big game animals (moose, 
white tailed deer, roe deer, wild boar, wolf, bear etc.) is 
gathered at the beginning of March by track index. The 
information dates back 20 years. Earlier the data was at hunting 
association level nowadays in hunting area level. The Finnish 
Hunting Association provided data, available as points 
representing individual moose observations. The inventory took 
place every year in beginning of March, representing winter 
habitats of moose. Datasets for the Uusimaa region, i.c. the 
Uusimaa game management district, are available from 1997 — 
2003. Starting from 2001, individual moose locations with x/y 
coordinates were inventoried as point data. 
Furthermore we were provided with road network data and 
wildlife accident records for 2002 from the Finnish road 
administration (FinRA ). 
2.2 Determination of the moose density 
To determine changes in the habitats of moose we calculate the 
moose density for different years using a Kernel interpolation 
method. Kernel estimation was originally developed to obtain a 
smooth estimate of a univariate or multivariate probability 
density from an observed sample of observations (Bailey & 
Gatrell, 1995). Given a random data sample, i.e. in our case 
moose population at defined locations, the probability 
distribution needs to be estimated. Applying a kernel to these 
statistical estimations is useful, as the method allows adjustment 
in cases of high variance from a ,,normal* distribution and the 
amount of smearing. This is made possible by an adjustable 
width of the kernel - with a wide kernel allowing for higher 
smoothing - and an adjustable bandwidth, influencing the 
amount of detail in the resulting plot (Silverman, 1986). 
For habitat modeling, kernel methods for bivariate data must be 
applied, building upon a bivariate function of data points 
representing individual moose observations on a plane — in our 
case the study area Uusimaa U. x is the number of moose of a 
total of n observations with each observation point s,. The 
density À at each observation point s is estimated by 
A(s)- p K(s-s)x sel 
i-l 
with K representing the kernel and // the bandwidth. The 
bandwith (4) for moose density habitats is set to a radius of 7.5 
km. It is based on an estimated moose movement radius in the 
winter time. 
Selecting an appropriate bandwidth is a critical step in kernel 
estimation. The bandwidth determines the amount of smoothing 
of the point pattern and defines the radius of the circle centered 
on each grid cell, containing the points that contribute to the 
density calculation. In general, a large bandwidth will result in 
a large amount of smoothing and low-density values, producing 
a map that is generalized in appearance. In contrast, a small 
bandwidth will result in less smoothing, producing a map that 
depicts local variations in point densities. (Bailey & Gatrell, 
1995). 
3. VISUALIZATION OF THE RESULTS 
3.1 Changes in the moose habitat data in combination with 
the road network 
We use the individual density maps for the years 2000 to 2003 
and overlay them with the road network. The road network data 
is available from 2002. Figure 4 a,b,c shows the moose density 
maps for the years 2001 to 2003 combined with the road 
network. 
  
  
2001 2002 
  
  
  
  
  
  
  
  
  
  
Figure 4. a,b,c - Moose density in winter 2001 to 2003 for 
Uusimaa, Finland. 
We take the calculated moose density as an indicator for the 
moose habitats in the winter season. To combine this data with 
the road network aims to visually indicate changes in the 
habitats caused by the road network. 
411 
 
	        
Waiting...

Note to user

Dear user,

In response to current developments in the web technology used by the Goobi viewer, the software no longer supports your browser.

Please use one of the following browsers to display this page correctly.

Thank you.