Initially
the factors controlling the spread of the Mountain Pine Beetle (MPB)
infestation had to be determined. This was entirely based on previous
studies,
mainly the study of Carroll et. al. (2006). The
following climatic
parameters were used to determine areas deemed suitable for the MPB.
PC1.
Minimum coldest month
temperature higher than -40ºC
PC2. Minimum 833
degree-days above
5ºC
PC3. Average
maximum August
temperature above 18.3ºC
PC4. Total spring
precipitation lower
than long term average.
The above criteria PC1,
PC2, PC3 and PC4
are
either true or false and were combined to estimate the areas suitable
for MPB
as follows:
PC:
PC1 ∧ PC2 ∧ PC3
∧ PC4 =
1. [1]
PC is
true (suitable, = 1) if, and only if, PC1,
PC2, PC3 and PC4
are all
true, and is false (unsuitable, = 0) otherwise (Carrol et al., 2006: 2).
Forest parameters:
PF1: Species
(Lodgepole pine)
PF2: Age
(80-160 years)
PF: PF1
∧ PF2 =
1. [2]
[1] and [2]
are then combined to determine the area suitable for MPB, i.e. climate
and
forest conditions both fit the MPB:
S: PS ∧
PF =
1. [3]
That is, S is
true (the area is suitable,
= 1) if, and only if, PS is true, (PC1,
PC2,
PC3 and PC4
are all true), and PF
is true (PF1
and PF2 are both true)
and false otherwise (i.e. the area is unsuitable for MPB, = 0).
GIS
method
Posted by Simon, Dec. 3rd., 2010.
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Study
area
In order to
limit the amounts of data as well as the calculation time, a smaller
part of BC
was chosen as our study area. It was decided to extend from
900000E-1350000E
and 1150000N-1450000N in the BC Albers Projection. This area was chosen
due to
its location at the northernmost outskirts of the MPB range, as well as
its
relatively high frequency of susceptible, but not yet infested trees as
well as
some areas already infested.
Practically, the layers were
limited to the
study area by setting the processing extend to the coordinates mentioned
above in geoprocessing environments.
See map of study area.
Forest
data
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Raster data
with forest
age and leading species was downloaded from HectaresBC as ASCII-files. The
ASCII-files were converted
into raster-files in ESRI ArcGIS (GIS) 10 using the ‘from
ASCII to Raster’
conversion tool.
Using the ‘define projection’ tool, the raster
layer was then assigned a spatial reference, 1983 NAD CSRS BC
Environment Albers.
After converting the files
to raster new values were assigned to the cells with the ‘reclassify’ tool.
The cells with trees in the susceptible age class (80-160 years old) in
the
forest age layer was assigned the value 1 and likewise were the cells
with Lodgepole
pine as the leading species in the leading species layer. All other
cells were
assigned the value 0.
Using the
’raster calculation’
tool, the two reclassed layers were multiplied to
create a new layer were cells with the value 1 contain trees in the
susceptible
age and species. The rest of cells with the value 0 were discarded off.
Flowchart, Forest
Climate
data
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The
ClimateBC software was downloaded from Climate BC. To
generate data to fit the
ClimateBC multiple location format, a DEM (1x1 km cells) was
reprojected to the
CSRS BC Environment Albers projection (define projection)
and multiplied
by 1 (raster calculator) to limit it to the study
area.
Secondly,
the DEM
containing the study area was converted into a point file and
reprojected to
decimal degrees in NAD1983 using the ’feature project’
tool in
the ’data management toolbox’.
Two
float-fields with the
header x and y, respectively,
were added in the attribute table
of the new DEM point layer. The x- and y-values were calculated in
these new
fields using the ’calculate geometry’ tool. The
attribute table was
exported as a dBASE-file (.dbf), opened in Microsoft Office Excel,
formatted to
the ClimateBC standard and saved as a comma delimited file (.csv). The
necessary climate data was then extracted with the ClimateBC software
using the
’multiple location’ function.
To
create raster layers
from the climate data it was imported back into GIS as X, Y coordinates
(decimal degrees) in NAD1983 with the climate parameter of interest as
z-value.
This was performed by right-clicking on the climate data table in
ArcCatalog
and choosing ’create feature class from
X,Y table’. These layers were then reprojected back to CSRS
BC Environment Albers
projection and converted from a point layer to a raster layer using ‘feature to raster’ tool. As the climate
data field is imported in double
format
we need to multiply it by 10 and use the ’int([layer])’
function in the raster calculator to turn it into integer data and
create an
attribute table.
Finally, these layers were
reclassified so all cells with the appropriate climate conditions are
assigned
the value 1 and all other cells were assigned the value 0 (see equation
1).
Flowchart, Climate Data
Susceptible
habitats
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To
determine the areas susceptible to a MPB infestation our two layers (climate
and forest) were multiplied so all cells with the value 1 in the
resulting
layer meets all the criteria specified, i.e. equation 3 is true: equals
1.