COS 13-4
Assessing a 60-year red spruce radial growth chronology relative to pollution critical load exceedance values

Monday, August 10, 2015: 2:30 PM
336, Baltimore Convention Center
Paul G. Schaberg, USDA Forest Service, Burlington, VT
Benjamin J. Engel, Rubenstein School of Environment and Natural Resources, University of Vermont, Burlington, VT
Gary J. Hawley, Rubenstein School of Environment and Natural Resources, University of Vermont, Burlington, VT
Shelly A. Rayback, Department of Geography, University of Vermont, Burlington, VT
Jennifer A. Pontius, Rubenstein School of Environment and Natural Resources, University of Vermont, Burlington, VT
Alexandra M. Kosiba, Rubenstein School of Environment and Natural Resources, University of Vermont, Burlington, VT
Eric K. Miller, Ecosystems Research Group, Inc., Norwich, VT
Background/Question/Methods

Acidic sulfur (S) and nitrogen (N) deposition depletes cations such as calcium (Ca) from forest soils and has been linked to increases in foliar winter injury that led to the decline of red spruce (Picea rubens Sarg.) in the northeastern United States. We used results from a 30 m resolution steady-state S and N critical load exceedance model for New England to better understand the spatial nature of the connections between Ca depletion and tree productivity. Atmospheric deposition and other inputs were estimated for a 5-year period (1984-1988) in order to smooth year-to-year variations in climate and patterns of atmospheric transport. Deposition levels prior to reductions that followed the 1990 Amendments to the Clean Air Act were used because tree health and productivity declines were expected to be most responsive to high acid loading. We examined how radial growth (basal area increment) of dominant and co-dominant red spruce trees across Vermont and New Hampshire was related to modeled estimates of S and N critical load exceedance.  Examining 60 years of annual radial growth for red spruce from 37 sites with a range of modeled exceedance values, statistical models were used to assess influences on growth including “year” and “elevation class” (to capture climatic variability), exceedance and interactions among these.

Results/Conclusions

Climate accounted for most of the modeled variation in growth. However, exceedance was significantly and negatively associated with mean growth for the study period (1951-2010) overall, and particularly for the 1980s and 2000s – periods of numerous and/or severe foliar winter injury events. Because high winter injury reflects the convergence of predisposing (cation depletion) and inciting (weather) factors, exceedance alone appears insufficient to define associated patterns of growth reduction. Significant interactions indicated that exceedance had little influence on growth at low elevations (where intrinsic conditions for growth were generally good) or high elevations (where growth was uniformly poor), whereas exceedance was significantly associated with reduced growth at mid elevations. Exceedance was also linked to reduced growth rebounds following a region-wide foliar winter injury event in 2003. Overall, our analyses suggest that modeled S and N critical load exceedance can help account for red spruce growth and rebound from injury in the field. Interestingly, recent growth for red spruce is above the average for the current dendrochronological record – indicating that the factors shaping growth may be changing. The influence of reduced pollution inputs on this recent growth surge is under investigation.