340 likes | 602 Views
Climatic and biophysical controls on conifer species distributions in mountains of Washington State, USA D. McKenzie, D. W. Peterson, D.L. Peterson USDA Forest Service, Pacific Northwest Research Station P. E. Thornton National Center for Atmospheric Research
E N D
Climatic and biophysical controls on conifer species distributionsin mountains of Washington State, USA D. McKenzie, D. W. Peterson, D.L. Peterson USDA Forest Service, Pacific Northwest Research Station P. E. Thornton National Center for Atmospheric Research
What are the impacts of spatial and temporal climatic variability on critical plant resources and species distribution? • What is the range of variability in biophysical environments of mountain landscapes across a marine-to-continental climatic gradient? • How would climate-driven changes in the biophysical environment affect species distribution?
Why model species distributions? • Plant community composition affects ecosystem properties and processes. • Forest management practices are often based on forest cover types. • Species have responded individually to past climatic changes.
Objectives • Define empirical environmental niches for major tree species in the Pacific Northwest. • Model changes in spatial distribution of environmental niches under future climate. • Identify core habitat areas, stress zones, and potential for speciesmigrations.
Forested Bioregions of the PNW Sitka spruce Western hemlock, Douglas-fir, and Western red cedar Pacific silver fir, subalpine fir and mountain hemlock Douglas-fir, grand fir Ponderosa pine, Douglas-fir Franklin and Dyrness 1973
Br. A. Brousseau – St. Mary’s College C. Webber – California Academy of Sciences
Methods (1) • Tree species data from Area Ecology Program. • 1-km climate coverages from DAYMET. • Biophysical variables computed from VIC and MT-CLIM.
Relative abundance of 6 key species along a geographic gradient
Methods (2) • Generalized linear models (GLMs) to predict probability of occurrence. • From proxy sets (correlated predictor variables), select no more than one. • Quadratic terms identify unimodal responses. • Models at multiple scales for each species. • Bootstrapped receiver operating characteristic (ROC) curves estimate accuracy and robustness.
Variables used to predict species distributions Summer = June, July, August, September. Winter = December, January, February. aSoil water indices were computed at three depths in the soil layer: 0-10 cm, 10-40 cm, and 40-100 cm.
PDE ~ steeper environmental gradients
Area under ROC curve represents the ability of the model to discriminate between presence and absence at all cut levels Grizzly bear – ponderosa pine All 4 forests – Engelmann spruce Area under ROC curve = 0.941 Area under ROC curve = 0.723
Probability of occurrence Probability of occurrence Ponderosa pine – Wenatchee NF Douglas-fir – Wenatchee/Grizzly Bear combined
Applications to modeling the effects of climatic change? • Is there a disconnect between scales? • 17 or 50 years of current climate predicts distributions in 75-300 yr-old forests. • Are equilibrium models useful? • Climate annual means and species presence/absence are snapshots. • What about “process-based” modeling?
Other dimensions of the problem • Competitive effects – species composition • Distribution (presence/absence) vs. abundance • Mature niche vs. regeneration niche
What forest types are most sensitive to climatic variability? Western red cedar Douglas-fir/grand fir Pacific silver fir Mean Productivity Douglas-fir mixed conifer Pacific silver fir/mountain hemlock Pacific silver fir/western hemlock Subalpine fir Annual Variability in growth Hessl et al.
Constraint lines representing limiting factors (Grizzly bear data) Ponderosa pine Douglas-fir Mountain hemlock Subalpine fir
Mature niche Regeneration niche Species 3 Species 1 Climate variable 2 Species 2 Climate variable 1 Species that currently coexist may not have equal capacity to regenerate under changing climate
Conclusions • Focus on climate and biophysical variables allows predictions under changing climate. • Models are consistent across scales – robust estimation of environmental niches. • More complete picture will emerge from complementary studies of abundance, composition, and regeneration.
Institutions Thanks! People • Amy Hessl • Dan Fagre • Bud Kovalchik • Robert Norheim