2.1. Model of Forest and Fire Dynamics
We built a non-spatial, deterministic system dynamics model of forest and fire dynamics, implemented on a hypothetical 1000 ha landscape. System dynamics models are generally defined by stocks (i.e., levels), flows (i.e., rates of transition in/out of stocks), and feedback loops. In this case, the stocks represent levels of each S-Class, flows represent succession- and disturbance-driven S-Class transitions, and feedback loops emerge from stock-flow relationships following the basic dynamics illustrated in
Figure 1 (although more complicated). We implemented the model using the VenSim for Windows Version 7.3.5 software (© Ventana Systems, Inc., Harvard, MA, USA).
We based our model on a state-and-transition model developed by the LANDFIRE program [
49,
50] (
https://www.landfire.gov/) to simulate long-run dynamics under a natural fire regime. LANDFIRE is a multi-partner governmental program that provides geospatial data describing vegetation, wildland fuel, and fire regimes across the United States. Data products provided by LANDFIRE have been used for a wide range of applications, including fire behavior modeling, fuel treatment prioritization, fire planning, and vegetation condition assessment. We were interested in LANDFIRE state-and-transition models of biophysical settings, which simulate the relative amount and transitions between S-Classes due to succession and disturbance. More information on LANDFIRE biophysical setting models, vegetation condition assessment, and departure modeling can be found in [
18,
29,
30] along with (
www.landfirereview.org).
Specifically, as described above, we selected the model developed for the “Southern Rocky Mountain Ponderosa Pine Woodland” biophysical setting (ID 10540). This biophysical setting covers large contiguous areas of ponderosa pine in the United States, characterized by low elevation, dry forest conditions with a frequent, low-severity fire regime. There are five primary S-Classes defined for this biophysical setting, which are broken down according to upper layer lifeform, height, and canopy cover (
Table 1 and
Table 2). Natural succession proceeds according to the following flows: A → C; B → E; C → D. Under reference conditions representative of a natural fire regime, S-Class D dominates the landscape, and tree cover greater than 60% is considered uncharacteristic (UN). We address transitions into our UN class, as well as their importance, in the following paragraphs.
The LANDFIRE model was developed to model system behavior under pre-suppression-era reference conditions, meaning it does not capture the accumulation of UN fuels due to fire exclusion. We therefore opted to add UN succession flows resulting from the accumulation of fuels due to fire suppression. These UN flows would occur contemporaneously with natural succession (NS) flows, but would instead add to stocks with denser forest conditions (i.e., A → B; C → B; D → E). Further, we opted to add a fuel accumulation multiplier for each S-Class to account for the rapid densification of forest and accumulation of fuels due to growth of understory (e.g., grass and shrubs), in addition to smaller diameter and shade-tolerant trees beneath the forest canopy. We mean rapid in a relative sense, in that the UN fuel accumulation may lead to changes in S-Class which are faster than natural succession transition times (see Figures 1 and 4 in [
35]).
Our model expanded the LANDFIRE state-and-transition model by considering the proportion of the 1000 ha landscape at any point in time that would be in one of multiple S-Classes. That is, instead of modeling S-Classes as state variables that may change in each time period, our model considers the dynamic behavior of stocks of S-Classes and the flows between them. In the original model, state transitions are due to probabilistic disturbances and deterministic (time-dependent) natural succession. We instead model flows between stocks with continuous rates, described below. The drawback is the loss of probabilistic variation, but the gains from changing to a stock-and-flow model are the abilities to evaluate the dynamics of distribution of S-Classes over time, and to capture nonlinear behavior emerging from interactions of succession and management.
In particular we were interested in fire-driven transitions, which are a function of burn severity. Whereas the state-and-transition model used specific burn rates for each S-Class state and burn severity combination, we were interested in applying a common burn rate to the entire landscape. In terms of model workflow, this means the exogenous (policy-driven) burn rate determines the total area of the landscape burned each year, while the endogenous distribution of S-Class stocks determined by forest and disturbance dynamics in turn determines the relative percentages of area burned at low, moderate, and high severity. To accomplish this, we simply derived conditional burn severity probabilities from the LANDFIRE model parameters (see
Table 3, described later).
Our modeling framework is designed as follows. First, we define the following parameters:
index for S-Class i
natural succession transition time (i.e., measured by years) for S-Class i
burn rate (i.e., annual burn rate) for S-Class i
user-defined fuel accumulation rate parameter for S-Class i. By setting , we would assume the S-Class i transfers into the corresponding UN class faster than the natural succession rate calculated as
Note that for our simulations, we kept the burn rate and fuel accumulation parameter constant across S-Classes, but retained generality for the formulation in case S-Class specific burn rates were defined later. Next, we defined equations for the uncharacteristic succession (UN) and natural succession (NS) flow rates:
In the baseline LANDFIRE model, UN flows are not modeled, which is equivalent to setting flow rate to zero, and the NS flow rate is the inverse of the natural succession transition time (i.e., a transition time of 50 years corresponds to an annual flow rate of 1/50). The logic behind calculating flow rate is based on the probability of the S-Class not experiencing fire (1 − BRi) over the duration of that transition time (hence the multiplication of this probability for Ti years). As the burn rate decreases, this compound probability increases, putting a larger proportion of the total stock outflow into the UN flow. Because the fuel accumulation parameter () could be set to greater than one, UN flows could exceed the value of (1/Ti), hence, the min operand in Equation (1).
In addition to UN flows, we also explored adding two UN stocks as new S-Classes, corresponding to the lower right portion of
Table 2. Specifically, we added (UNB), similar to B but with canopy cover > 60%, and (UNE), similar to E but with canopy cover > 60%. The new UN flows into these new S-Classes are B → UNB and E → UNE, which are similarly calculated according to Equations (1) and (2). In a preliminary analysis, we developed five model formulations that varied according to whether UN flows were included, whether UN stocks were included, and whether the fuel accumulation parameter was set to 1.0 or 2.0.
Appendix A contains more detailed results on comparative analysis of alternative model formulations. We ultimately opted to use the model with both UN stocks and UN flows, and a fuel accumulation parameter of 2.0 (UNS-fa-2; see
Appendix A); the results for all policy and scenario analysis correspond to this model formulation.
The dynamics underlying all of the succession- and disturbance-driven flows used in our model are depicted in
Figure 3 and summarized with more detail in
Table 3. The figure also illustrates the role of the burn rate and fire response policy variables, which, for simplicity, we only show for S-Class C. The connections between
Figure 3 and the stylized causal loop diagram in
Figure 1, which stem directly from the underlying model structure, can be explained as follows. First, as the burn rate decreases, the UN flow rates increase, shifting the S-Class distribution towards denser stocks. The net effect for S-Class C would be relatively lower NS flow rates into S-Class D (open forest) and higher UN flow rates into S-Class B (closed forest). This shift to denser forest stocks in turn results in comparatively higher conditional rates of high-severity fire (e.g., 0.21 for S-Class B versus 0.02 for S-Class D;
Table 3), which eventually lead to greater rates of transition into S-Class A. With a lower burn rate, S-Class A then has relatively higher flow rates into S-Class B (UN flow) instead of back into S-Class C (NS flow), which further sets the landscape on a trajectory of denser forests with higher conditional rates of high fire severity. Further, as we explore in policy resistance scenarios (described below), increased rates of high-severity fire and corresponding increases in S-Class A can lead to policy responses which are geared towards fire exclusion, creating a reinforcing loop.
We made no changes to preexisting LANDFIRE transition times or non-fire disturbance rates. Further, we did not adjust any LANDFIRE pathways labeled as “alternative succession,” which reflect underlying forest dynamics that may result in transitions distinct from NS pathways (i.e., these are considered separate from our UN flows). As described in the
Appendix A, we did estimate new conditional burn severity probabilities for fire-related flow rates for the new UN stocks. The D, E, and UNE stocks have no NS flows, although D and E both have UN flows into denser stocks (E and UNE, respectively). The UNE stock can only be reduced through burning at moderate and high-severity fire. In all cases, low-severity fire maintains the stock, and sometimes moderate severity fire does as well. Within the model, fire that maintains the S-Class is not directly modeled as a flow that changes stock levels, but we track these to account for fire severity over time.
The area burned at high severity is jointly determined by the burn rate, S-Class distribution, and S-Class conditional fire severity probabilities. The lower bound is a landscape composed entirely of S-Class A, which for any burn rate would result in 0 ha of high-severity fire. The upper bound results from a landscape composed entirely of S-Class UNE, which for a burn rate of 0.1 (100 ha out of 1000 ha burned) would result in 40 ha burned. The spectrum of S-Class distributions in between these two extremes dictates the actual amount of area burned at high-severity fire in any simulation year.
2.2. Wildfire Response Policy Scenarios
We initially designed a total of seven wildfire response policy scenarios, which include a status quo (SQ) policy along with six alternative policies (
Table 4). For simulation purposes, all policies begin from steady state conditions (2000-year simulation, 10-year MFRI, 0.1 burn rate), and are simulated over a 250-year time horizon. Specifically, we simulate 50 years of a natural fire regime (10-year MFRI, 0.1 burn rate) then 100 years of fire exclusion (80-year MFRI, 0.0125 burn rate) before initiating changes in response policy. All response policies are implemented for a duration of 100 years. The exception is the Status Quo (SQ) policy of fire exclusion (80-year MFRI), which is implemented consistently over a 200-year time horizon after the 50 years of the natural fire regime. The alternative response policies are defined by two key variables, i.e., target mean fire return interval (MFRI) and target attainment time, which correspond to the scale and pace of the restoration strategy. The labeling schema for these alternative policies is: “Target MFRI-Target Attainment Time.” We designed these strategies to cover a range of managerial preferences, ranging from what we colloquially label “Hot and Fast” (10-10) to “Cool and Slow” (40-40), with a spectrum of combinations in between. The complete set of policies we evaluated is: 10-10, 10-40, 20-20, 30-30, 40-10, and 40-40.
We evaluated policy performance in terms of departure from steady state conditions, amount of high-severity fire, and time to restore D and E. For the former, we calculated mean values of total departure as well as the UNE stock as indicators of degraded forest conditions (UNB stocks, while also an indicator of degraded conditions, are generally very low due to low initial levels of B). For simplicity we calculate departure as the absolute deviation of current S-Class area from initial reference conditions, summed over all S-Classes. We also kept track of whether individual S-Class status would be considered surplus, similar, or deficit, where the surplus (deficit) threshold is defined as being greater than +33% from reference conditions (less than −33%). For severity, we reported both percentage and area burned at high severity. We define “time to restore” as the time at which S-Class stocks are returned to similar status; for D, this is a return from deficit, and for E, this is a return from surplus.
Lastly, we evaluated the potential for policy resistance, wherein unintended or undesirable consequences from changing fire policy could induce pressures that inhibit change (
Table 5). We used the presence of a surplus of A (a proxy for excessive high-severity fire) as a trigger to initiate policy resistance, and considered two policy resistance scenarios: “CS,” which reverts to the “Cool and Slow” policy of 40-40, and “SQ,” which reverts to the SQ fire exclusion policy (i.e., 80-1). The response policy (i.e., the burn rate, or equivalently the MFRI) reverts to the original policy anytime A is no longer in surplus. Only response policies 10-10 and 10-40 triggered policy resistance.