This map represents the percent change in average annual
vapor pressure deficit, simulated by the model MC1 between the 30-year periods 1971-2000
and 2070-2099, using the Hadley projected climate and A2 emissions scenarios.
The average annual vapor pressure deficit for the respective 30-year periods
decreased in all of the 5,311 grid cells of the Eastern Oregon study area.
The greatest decrease was -33.04%; the least decrease was --40.97%; and the mean
decrease was --36.49%
The vegetation model MC1 (e.g. Bachelet et al. 2001) was used to simulate
vegetation dynamics, associated carbon and nitrogen cycle, water budget, and
wild fire impacts at two study sites, one in eastern Oregon (Deschutes and
Fremont-Winema National Forests) and one in Arizona (Apache-Sitgreaves National
Forest area). The work was funded by the USDA Forest Service (PNW
09-JV-11261900-003). Historical climate input data used to run the model were
provided by the PRISM group (Chris Daly, OSU) at 30 arc-second (~800m) spatial
grain. The model was also run using future climate change projections from
three general circulation models: Hadley, CSIRO Mk3 and MIROC 3.2 medres.
Future climate datasets were generated through statistical downscaling from
general circulation model output using a simple anomaly method and the
climatology (1971-2000) from the PRISM group at 30 arc-second spatial
grain. The model was run assuming that nitrogen demand from plants is
always met, so that the nitrogen concentrations in various plant parts never
drop below their minimum reported values. A CO2 enhancement effect increases
productivity and water use efficiency as atmospheric CO2 concentration
increases.