Empirical Modeling of Atmospheric Deposition in Mountainous Landscapes
Weathers KC, Simkin SM, Lovett GM, Lindberg SE. 2006. Empirical Modeling of Atmospheric Deposition in Mountainous Landscapes. Ecological Applications. 16(4):1590-1607
' Atmospheric deposition has long been recognized as an important source of pollutants and nutrients to ecosystems. The need for reliable, spatially explicit estimates of total atmospheric deposition (wet + dry + cloud) is central, not only to air pollution effects researchers, but also for calculation of input-output budgets, and to decision makers faced with the challenge of assessing the efficacy of policy initiatives related to deposition. Although atmospheric deposition continues to represent a critical environmental and scientific issue, current estimates of total deposition have large uncertainties, particularly across heterogeneous landscapes such as montane regions. We developed an empirical modeling approach that predicts total deposition as a function of landscape features. We measured indices of total depositions to the landscape of Acadia (121km2) and Great Smoky Mountains (2074 km2) National Parks (USA). Using ~300-400 point measurements and corresponding landscape variables at each park, we constructed a statistical (general linear) model relating the deposition index to landscape variables measured in the field. The deposition indices ranged over an order of magnitude, and in response to vegetation type and elevation, which together explained ~40% of the variation in deposition. Then, using the independent landscape variables available in GIS data layers, we created a GIS-relevant statistical nitrogen (N) and Sulfur (S) deposition model (LandMod). We applied this model to create park-wide maps of total deposition that were scaled to wet and dry depostion data from the closest national network monitoring stations. The resultant deposition maps showed high spatial heterogeneity and a four- to six fold variation in ôhot spotsö and ôcold spotsö of N and S deposition ranging from 3 to 31 kg N╖ha 1╖yr-1 and from 5 to 42 kg S╖ha1╖yr1 across these park landscapes. Area-weighted deposition was found to be up to 70% greater than NADP plus CASTNET monitoring-station estimates together. Model validation results suggest that the model slightly overestimates deposition for deciduous and coniferous forests at low elevation and underestimates deposition for high-elevation coniferous forests. The spatially explicit deposition estimates derived from LandMod are an improvement over what is currently available. Future research should test LandMod in other mountainous environments and refine it to account for (currently) unexplained variation in deposition. ' /STUDY LOCATIONS:/ /ACADIA NATIONAL PARK/
- Type
- Journal Article
- Authors
- Weathers, Kathleen; Simkin, Samuel; Lovett, Gary; Lindberg, Steven
- Units
- ACAD , ARD , GRSM
- Keywords
- Acadia National Park, AIRBIB, ARD_Park-Air-Info_Collection, Atmospheric Deposition, Deposition, Elevation, empirical modeling (LandMod), Geographic Information Systems (GIS), Great Smoky Mountain National Park, GRSM-00002, GRSM-00192, Hotspots, landscape features, Model, Modeling, Monitoring, Nitrogen (N), Sulfur (S), throughfall, Vegetation Type