Predicted probability of marten summer occurrence created
with Maxent (Phillips et al. 2006) using marten detections (N = 197, May –
November, spanning 1990 – 2011) and nine predictor variables: mean potential
evapotranspiration, mean annual precipitation, mean summer temperature
amplitude, mean fraction of vegetation carbon burned, mean forest carbon (g C m2),
mean fraction of vegetation carbon in forest, understory index (fraction of
grass vegetation carbon in forest),
average maximum tree LAI, and modal vegetation class. Predictor
variables had a grid cell size of 4 km by 4 km, vegetation variables were
simulated MC1 dynamic global vegetation model (Bachelet et al. 2001) and historical
climate variables were provided by the PRISM GROUP (Daly et al. 1994). This
marten distribution model has a 10-fold cross-validated AUC of 0.860 +/- 0.021
and was generated as part of a pilot project to apply and evaluate the Yale
Framework (Yale Science Panel for Integrating Climate Adaptation
and Landscape Conservation Planning).
Grid Value Predicted
Probability of Occurrence
1
0 – 0.2
2
0.2 – 0.4
3
0.4 – 0.6
4
0.6 – 0.8
5
0.8 – 1.0
References:
Bachelet D., R.P. Neilson, J. M.
Lenihan, and R.J. Drapek. 2001. Climate change effects on vegetation
distribution and carbon budget in the U.S. Ecosystems 4:164-185.
Daly, C., R.P. Neilson, and
D.L. Phillips. 1994. A statistical topographic model for mapping climatological
precipitation over mountainous terrain. Journal of Applied Meteorology
33:140–158.
Phillips, S.J., R.P. Anderson, and R.E. Schapire. 2006. Maximum
entropy modeling of species geographic distributions.
Ecological
Modelling 190: 231-259.
Note: The MC1 model is described in data basin (http://databasin.org/climate-center/features/mc1-dynamic-global-vegetation-model).