Frequently Asked Questions

Q: When will model/results be available?

Q: How does this model differ from the Chesapeake Bay HSPF (Hydrological Simulation Program - FORTRAN) Model?

Q: Does the model allow us to set or achieve some level of economic viability and see the resulting level of ecological health?

Q: Can the information be extrapolated beyond the Patuxent watershed?

Q: Why didn't you use an existing (hydrology) model?

Q: Does your model include atmospheric inputs of nutrients?

Q: How is the model calibrated?

Q: Why do you inter-calibrate the model with EPIC (Erosion Productivity Impact Calculator) instead of using EPIC directly?

Q: What types of ecological indices can be calculated with the model?


Q: When will model/results be available?

A: Ecological Model

Preliminary scenario results should be available in 6 months.

The web site displays model structure and results and allows people to interact with the broader management/research community.

The model code is publicly available for those wanting to run their own model, however, the model requires very poweful hardware, currently runs only under UNIX, and may be too complex for many people to run.

Plans are being considered that would use the graphic user interface to offer sets of model options (scenarios) that could be controlled and run by an unsophisticated user.

A: Economic Model

Results could be generated by this spring. In one year from this summer the model will be about as good as the data allow. Some questions such as effects of agricultural policies will be poorly represented by the model at that time because much spatially explicit agricultural data (e.g. farm practices, profitability) is kept confidential, preventing estimation of farmer decisions in response to policy change. Improved data is being developed and may enhance future estimations of farmer's decisions.

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Q: How does this model differ from the Chesapeake Bay HSPF (Hydrological Simulation Program - FORTRAN) Model?

A: Our model differs in two fundamentally different ways:

  1. The spatial resolution is finer. Whereas in HSPF a weighted average of land use types and conditions is used to characterize each subwatershed, we divide the watershed into equal size grid cells which are smaller than the subwatersheds used in HSPF. Each cell has one habitat/land cover type assigned to it, based on the dominant land use within that cell. The habitat type is linked to a database of model parameters for such processes as potential plant growth rate. Each grid cell is linked to a set of information about soil type, elevation, etc. for that particular point on the landscape. This allows land use type and the associated parameters to be changed easily and better represents spatial distribution on the landscape, which is essential for many ecological processes and the economic linkages.
  2. The model includes dynamics between plant and animal communities on land and nutrient and hydrologic processes. HSPF does not explicitly model plant and animal communities.
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Q: Does the model allow us to set or achieve some level of economic viability and see the resulting level of ecological health?

A: Yes, in the sense that we can set growth levels and examine changes to ecosystem indicators of health. We can also assess how policies alter land use distribution on the landscape which can impact ecosystem health. However, we need to assume a set of policies in order to test effects and can not work directly from the goal.

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Q: Can the information be extrapolated beyond the Patuxent watershed?

A: The economic model can be implemented for all counties encompassing the watershed, but would not be valid for other areas. The ecological model has been applied to other ecosystems, but the particular findings of the linked ecological economics model would not necessarily apply to other watersheds. General ecological or economic modeling techniques which are being developed will be widely applicable to data in other regions.

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Q: Why didn't you use an existing (hydrology) model?

A:For one, we could not find an off-the-shelf product that would suit all the needs of our integrated study. Our goal of incorporating land use change within the framework of the model required a fine scale partitioning of the landscape over fairly large areas. At the same time the model had to be simple enough to add other ecological and economic modules without the model becoming unwieldy.

On the other hand, we did use many already existing and tested hydrologic equations to represent the various processes in our model (Darcy's law, Manning's equation, etc.). There is nothing completely new and unproven in the formalism that we apply.

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Q: Does your model include atmospheric inputs of nutrients?

A: Yes it does. Nitrogen is imported into the landscape model via rain water (wet deposition) and through deposition of particles (dry deposition). Phosphorous is only imported through wet deposition. Rates for dry deposition increase when structure such as buildings or trees are present.

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Q: How is the model calibrated?

A: Finding the correct parameter values in such a complex model is a daunting task for a researcher. So, we have developed a computer-based algorithm which uses a custom Model Performance Index (MPI). Basically, the computer does a number of "eyeballing" runs comparing the available data and boundary or frequency conditions (e.g. maximum values or seasonal cycles) with the model's output for different sets of parameters. The parameter values are not selected randomly (as in a Monte Carlo technique) since the chance of finding the "good" points in such a big parameter space would be too small. Rather, the algorithm improves its search strategy by analyzing the results of each change and running statistical analyses at every step. This allows us to find acceptable parameter combinations in a reasonable time, much better than any human operator or any random algorithm could do. Additionally, the data gathered to improve the search strategy are of great value for improving the knowledge of the model's performance, as well as to quantify the benefit of using additional data which increases model costs.

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Q: Why do you inter-calibrate the model with EPIC (Erosion Productivity Impact Calculator) instead of using EPIC directly?

A: EPIC is a model specifically designed to characterize agricultural production. It is more complex and includes many more parameters related specifically to agricultural land use than our more generalized unit model could handle given the complexity of the whole model. Due to EPIC's relatively low error margin (7-10%) on estimates of crop growth and nutrient uptake rates, it can be used to calibrate the output of the unit model for agricultural land use. This enables us to understand the consequences of simplifying the agricultural model and helps identify ways to reduce error in the simpler model.

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Q: What types of ecological indices can be calculated with the model?

A: A large variety of indices can be calculated directly from model output including ones concerning: hydrologic flow variability, nutrient levels, plant productivity, pattern and proportion of land use, erosion, and general ecosystem health. A linked deer model will be able to estimate indicators related to deer population such as the probability of deer-car encounters.

We are also developing statistical models which link simulation model output to information about higher trophic levels such as fish. We hope our continued work with the model will show us important links in the system which are critical to ecosystem function and the provision of valuable services.

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