You are here
Harvard Forest Symposium Abstract 2017
- Title: Timing and local water balance regulate drought impacts on the temperate forest carbon sink
- Primary Author: Loic D'Orangeville (University of New Brunswick)
- Additional Authors: Daniel Bishop (Harvard Forest); Shawn Fraver (University of Maine); Neil Pederson (Harvard Forest); Richard Phillips (Indiana University - Bloomington); Christine Rollinson (Oberlin College)
- Abstract:
Loïc D’Orangeville, Indiana University, Bloomington, IN, loicdorangeville@gmail.com
Justin Maxwell, Indiana University, Bloomington, IN, maxweljt@indiana.edu
Daniel Kneeshaw, Université du Québec à Montréal, Montreal, Canada, kneeshaw.daniel@gmail.com
Neil Pederson, Harvard Forest, Harvard University, Petersham, MA, neilpederson@fas.harvard.edu
Louis Duchesne, Ministère des Forêts, Montreal, Canada, Louis.Duchesne@mffp.gouv.qc.ca
Travis Logan, Ouranos, Montreal, Canada, logan.travis@ouranos.ca
Daniel Houle, Ministère des Forêts, Montreal, Canada, Daniel.Houle@mffp.gouv.qc.ca
Dominique Arseneault, Université du Québec à Rimouski, Rimouski, Canada, dominique_arseneault@uqar.ca
Colin M Beier, State University of New York College of Environmental Science and Forestry, Syracuse, NY, cbeier@esf.edu
Daniel A. Bishop, Lamont-Doherty Earth Observatory, Palisade, NY, dbishop@fas.harvard.edu
Daniel Druckenbrod, Rider University, Rider, NJ, ddruckenbrod@rider.edu
Shawn Fraver, University of Maine, Bangor, ME, shawn.fraver@maine.edu
François Girard, Université de Montréal, Montreal, Canada, francois.girard@umontreal.ca
Joshua Halman, University of Vermont, Burlington, VT, joshua.halman@vermont.gov
Chris Hanson, University of Vermont, Burlington, VT
Justin L. Hart, University of Alabama, Tuscaloosa, hart013@ua.edu
Henrik Hartmann, Max Planck Institute for Biogeochemistry, Jena, Germany, hhart@bgc-jena.mpg.de
Margot Kaye, Pennsylvania State University, Happy Valley, PA, mwk12@psu.edu,
David Leblanc, Ball State University, Muncie, IN, dleblanc@bsu.edu
Stefano Manzoni, Stockholm University, Stockholm, Sweden, stefano.manzoni@natgeo.su.se
Shelly Rayback, University of Vermont, Burlington, VT, Shelly.Rayback@uvm.edu
Christie Rollinson, Pennsylvania State University, Happy Valley, PA, crollinson@mortonarb.org
Richard P. Phillips, Indiana University, Bloomington, IN, rpp6@indiana.edu
Drought can have a significant impact on the terrestrial carbon sink. While theory suggests that the specific hydraulic traits of dominant tree species can determine how forests respond to drought, some evidence suggests environmental drivers might be at in determining forest sensitivity. To test these ideas, we used a network of 10,753 trees across much of the mesic temperate biome of eastern North America (ENA) to determine what might drive the growth of trees. Importantly, our network is composed of 24 species, 452 populations, and collections of trees that might be more representative of the forest in which they grow compared to most studies conducted at this spatial scale. We found that mean evaporative pressure and the timing of drought are stronger drivers of drought sensitivity than soils, stand characteristics, or plant traits across species, time, and space. June is critical over the latitudinal gradient of our network, matching the seasonality of radial growth. Further, trees growing on drier sites (defined by their high summer evapotranspiration, PE) experienced the largest growth reductions during drought. If projected increases in PE increase forest sensitivity to drought, the gross C uptake of ENA’s temperate forest might decline by 5.2-8.2% annually. This increased sensitivity might overwhelm potential benefits of longer growing seasons, land use, rising atmospheric CO2, or nitrogen fertilization. - Research Category: Regional Studies
International Research Projects
Historical and Retrospective Studies
Forest-Atmosphere Exchange
Conservation and Management