OOS 17-4 - When dispersal fails to be followed by establishment: An example which has implications for patch dynamics

Wednesday, August 14, 2019: 2:30 PM
M104, Kentucky International Convention Center
Edward A. Johnson, Biogeoscience Institute, University of Calgary, Calgary, AB, Canada and Anzala Murtaz, Dept. Biological Sciences, University of Calgary, Calgary, AB, Canada
Background/Question/Methods: In boreal and subalpine forests vegetation dynamics is determined by large crown fires with small patch dynamic being less important. These small openings (1 to 4 tree heights) in subalpine and boreal forests at northern latitudes have deeper snow accumulation than large openings and closed canopied forests. This snow persists into the spring, and despite seed dispersal prevents regeneration of trees in these small opening. First, we give empirical evidence for persistent snow in small openings and no tree regeneration. Next, we use coupled mass (snow)-heat budgets over different sizes of forest openings to show the size of openings that cause snow accumulation and late spring melt.

Results/Conclusions: The empirical evidence of no tree regeneration is from more than 100 openings of ~1 to 4 tree heights in diameter. These small gaps were created more than 50 years ago by hydrologists to increase snow accumulation and extend the spring melt to increase spring runoff. Other openings greater than ~4 tree heights in diameter (wildfires) have trees recruit within 5 years of the opening being created. In the small openings the apparent reason no trees have re-established is the persistence of more than 1 to 2 meters of snow into the spring so that tree seedlings have a much-reduced growing season and are often infected by snow fungus (spp.). The processes that explain the snow accumulation are: 1) in small openings the low sun angle (in these northern latitudes) and surrounding canopy height shade the shortwave radiation from reaching into these small openings while the outgoing longwave radiation has no barrier to the sky, producing a cold hole which allows snow to accumulate; 2) in large openings both shortwave and longwave radiation contribute to snow melt; 3) in closed canopies longwave radiation dominates causing surface snow melt, and shortwave radiation causes snow caught in the conifer canopies to be lost by sublimation. This snow accumulation and delayed melt in small openings is at least one explanation for not finding patch dynamics in these northern forests. Southern deciduous and northern hardwood forests do not have snow accumulation in small openings because higher sun angles and the mostly leafless trees in winter allow more shortwave radiation to penetrate to the forest floor and melt the snow.