MC1 is a widely used dynamic global vegetation model (DGVM) that has been used to simulate potential vegetation shifts in California and Alaska, all of North America, and over the entire globe under various climate change scenarios. However, past simulations were run at a scale that is too coarse (e.g., 10km x 10km for the California simulations) for use by local resource managers, such as those in Yosemite National Park ( see Data Basin feature on Yosemite results ). More recently, the model has been implemented at a finer resolution (800m x 800m) of greater utility to National Park staff.
MC1 is a model that simulates vegetation types, ecosystem fluxes of carbon, nitrogen, and water, as well as wildfire occurrence and impacts. MC1 is routinely implemented on spatial data grids of varying resolution (i.e., grid cell sizes ranging from 900 m2 to 2500 km2). The model reads climate data at a monthly time step and calls interacting modules that simulate:
The biogeochemistry module is a modified version of the CENTURY model , which simulates plant productivity, organic matter decomposition, and water and nutrient cycling once the vegetation type has been determined by the biogeography module. Plant growth is determined by empirical functions of temperature, moisture, and nutrient availability which decrement set values of maximum potential productivity. Plant growth is generally assumed not to be limited by nutrient availability. The direct effect of an increase in atmospheric carbon dioxide (CO2) is simulated using a beta factor that increases maximum potential productivity and reduces the moisture constraint on productivity. Grasses compete with woody plants for soil moisture and nutrients in the upper soil layers where both are rooted, while the deeper-rooted woody plants have sole access to resources in deeper layers. The growth of grasses may be limited by reduced light levels in the shade cast by woody plants. The values of model parameters that control woody plant and grass growth are adjusted with shifts in the lifeform mixture determined annually by the biogeography module. Plant parts simulated include leaves, fine branches, coarse branches and boles, fine and coarse roots. Litter pools include surface litter and standing dead, belowground litter and 3 soil carbon organic matter pools with increasing degrees of resistance to decomposition based on their chemical composition.
The fire module simulates the occurrence, behavior, and effects of fire. It simulates the behavior of a fire event in terms of the potential rate of fire spread, fireline intensity, and the transition from surface to crown fire. Several measurements of the fuel bed are required for simulating fire behavior, and they are estimated by the fire m 
odule using information provided by the other two MC1 modules. The current lifeform mixture is used by the fire module to select factors that allocate live and dead biomass into different classes of live and dead fuels. The moisture content of the two live fuel classes (grasses and leaves/twigs of woody plants) are estimated from moisture at different depths in the soil provided by the biogeochemical module. Dead fuel moisture content is estimated from climatic inputs to MC1 using different functions for each of four dead fuel size-classes. Fire events are triggered in the model when the moisture content of coarse woody fuels, and the flammability of fine fuels all meet set thresholds. Sources of ignition (e.g., lightning or anthropogenic) are assumed to be always available. Area burned is not simulated explicitly as fire spread within a given cell. Instead, the fraction of a cell burned by a fire event is estimated as a function of set minimum and maximum fire return intervals for the dynamically-simulated vegetation type and the number of years since a simulated fire event. Simulated fire effects include consumption and mortality of dead and live vegetation carbon, which is removed from (or transferred to) the appropriate carbon pools in the biogeochemistry module. Live carbon mortality and consumption are simulated as a function of fireline intensity and the tree canopy structure, and dead biomass consumption is simulated using functions of fuel moisture that are fuel-class specific.
The model has been used in various research projects since 1995 and summary results from various publications are being made available on Data Basin through a joint project between the USFS PNW and Conservation Biology Institute.
Most publications that include MC1 results are listed and made available HERE .
The model was originally designed by a team of OSU scientists (C. Daly, J. Lenihan, and D. Bachelet) in collaboration with the Century group in the Natural Resource Ecology Laboratory at Colorado State, with USFS-PNW financial support within Ron Neilson's MAPSS team. Several programmers (e.g. Jesse Chaney, David Conklin) contributed to the various versions of MC1 used in the published reports. It is currently maintained and documented by a group of Conservation Biology Institute scientists.
Collaboration has been established with a newly established group of MC1 developers communicating improvement to the code to the overall MC1 users community , and making available the latest version of the code on the OSU subversion repository .
