Abstract
Ultimately, our interest in ecological
thresholds is likely to be focused on evaluating changes in ecosystem
function. In many cases, however, atmospheric fluxes of pollutants and
nutrients are the critical drivers of those changes. The idea is not
new; since the 1990s approximately two-dozen European Community (EC)
countries have been using the so-called "critical loads" approach-essentially
identifying and setting the thresholds for ecological response to pollutant
deposition-to guide policy for emissions reductions. The EC community's
efforts at broad-scale monitoring in which they link emissions to deposition
to thresholds of ecosystem response, and their new focus on interactions
among elements, may provide insight and context for the consideration
of thresholds in ecological systems here in the US. Although we know
something about ecosystem response to disturbances such as eutrophication
and acidification within specific systems, total atmospheric deposition
is poorly described in the US at many spatial scales and for many types
of landcover and landuse. Furthermore, it can vary by 300% over small
(10s of meters) and large (1000s of kms) spatial scales as a result
of multiple atmospheric thresholds and the interactions between and
among atmospheric processes, landscape structure, and depositional inputs.
Understanding the different drivers of atmospheric deposition from spatial
scales that range from tens of meters to kilometers may help in identifying
geographically explicit regions where terrestrial and aquatic threshold
responses may occur.