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Soil residual water corresponds to the model variable "total
streamflow." In the model MC1, this is calculated (in cm of water)
as the water flowing through the soil profile below the last soil layer
(streamflow), water leached into the subsoil (baseflow) and also
includes runoff. The output is presented here as a monthly average. Soil
residual water is part of the model output from Brendan Rogers' MS
thesis work. Brendan used the vegetation model MC1 to simulate
vegetation dynamics, associated carbon and nitrogen cycle, water budget
and wildfire impacts across the western 2/3 of the states of Oregon and
Washington using climate input data from the PRISM group (Chris Daly,
OSU) at a 30arc second (800m) spatial grain. The model was run assuming
that nitrogen demand from the plants was always met so that the nitrogen
concentrations in various plant parts never dropped below their minimum
reported values. A CO2 enhancement effect increased productivity and
water use efficiency as the atmospheric CO2 concentration increased.
Data Provided By:
Brendan Rogers, MS Thesis
Content date:
1971,2000
Citation:
Title: Total soil residual water simulated in cm for January for the Pacific Northwest, USA (1971-2000 average) Credits: Brendan Rogers, MS Thesis Publication Date: 05/20/2010
Layers in this dataset are based on combinations of the following options.
You may choose from these options to select a specific layer on the map page.
The Conservation Biology Institute (CBI) provides scientific expertise to support the conservation and recovery of biological diversity in its natural state through applied research, education, planning, and community service.