Assessing the occurrence, vulnerability, expansion and disturbance of forests of the Pacific Northwest in response to recent climate variation Nicholas.

Slides:



Advertisements
Similar presentations
Site and Stocking and Other Related Measurements.
Advertisements

Land Surface Evaporation 1. Key research issues 2. What we learnt from OASIS 3. Land surface evaporation using remote sensing 4. Data requirements Helen.
Mapping of stress on native tree species across western U.S.A. & Canada: interpretation of climatically-induced changes using a physiologically-based approach.
Do In and Post-Season Plant-Based Measurements Predict Corn Performance and/ or Residual Soil Nitrate? Patrick J. Forrestal, R. Kratochvil, J.J Meisinger.
A Simple Production Efficiency Model 1/18 Willem de Kooning ( ) A Tree in Naples.
Gridded Biome-BGC Simulation with Explicit Fire-disturbance Sinkyu Kang, John Kimball, Steve W. Running Numerical Terradynamic Simulation Group, School.
Scaling Biomass Measurements for Examining MODIS Derived Vegetation Products Matthew C. Reeves and Maosheng Zhao Numerical Terradynamic Simulation Group.
Potential Change in Lodgepole Pine Site Index and Distribution under Climate Change in Alberta Robert A. Monserud Pacific Northwest Research Station, Portland,
The C budget of Japan: Ecosystem Model (TsuBiMo) Y. YAMAGATA and G. ALEXANDROV Climate Change Research Project, National Institute for Environmental Studies,
The Effects of Site and Soil on Fertilizer Response of Coastal Douglas-fir K.M. Littke, R.B. Harrison, and D.G. Briggs University of Washington Coast Fertilization.
Monitoring Effects of Interannual Variation in Climate and Fire Regime on Regional Net Ecosystem Production with Remote Sensing and Modeling D.P. Turner.
SKYE INSTRUMENTS LTD Llandrindod Wells, United Kingdom.
Climate Change Impacts on the Water Cycle Emmanouil Anagnostou Department of Civil & Environmental Engineering Environmental Engineering Program UCONN.
Mapping of stress on native tree species across western U.S.A. & Canada: interpretation of climatically-induced changes using a physiologically-based approach.
CALIBRATION 3-PG – Pinus pinaster Elemer Briceño 15/07/2008.
Climatic and biophysical controls on conifer species distributions in mountains of Washington State, USA D. McKenzie, D. W. Peterson, D.L. Peterson USDA.
Climate Change and Douglas-fir Dave Spittlehouse, Research Branch, BC Min. Forest and Range, Victoria.
4. Testing the LAI model To accurately fit a model to a large data set, as in the case of the global-scale space-borne LAI data, there is a need for an.
Questions How do different methods of calculating LAI compare? Does varying Leaf mass per area (LMA) with height affect LAI estimates? LAI can be calculated.
Climatic variability, land-cover change, and forest hydrology in the Pacific Northwest David W. Peterson JISAO Climate Impacts Group Forest Hydrology.
Bird diversity: A predictable function of satellite-derived estimates of seasonal variation in canopy light absorbance across the United States Nicholas.
Forrest G. Hall 1 Thomas Hilker 1 Compton J. Tucker 1 Nicholas C. Coops 2 T. Andrew Black 2 Caroline J. Nichol 3 Piers J. Sellers 1 1 NASA Goddard Space.
A Tool for Estimating Nutrient Fluxes in Harvest Biomass Products for 30 Canadian Tree Species CONTEXT: With a growing interest in using forest biomass.
Biodiversity Potential in the Pacific and Inland Northwest: Phase II – Applications to Industry Planning Areas Since the workshop on Boise: Now 16 months.
Tools for Protected Area Managers: Ecological Forecasting Within NASA Gary Geller Jet Propulsion Laboratory California Institute of Technology Edgemont.
An empirical model of stand GPP with LUE approach: analysis of eddy covariance data at several contrasting sites A. Mäkelä 1, M. Pulkkinen 1, P. Kolari.
1 Remote Sensing and Image Processing: 9 Dr. Hassan J. Eghbali.
A process-based, terrestrial biosphere model of ecosystem dynamics (Hybrid v. 3.0) A. D. Friend, A.K. Stevens, R.G. Knox, M.G.R. Cannell. Ecological Modelling.
UW-Milwaukee Geography Phenological Monitoring: A key approach to assessing the impact of spring starting earlier Mark D. Schwartz Department of Geography.
Enhanced Ecosystem Productivity in Cloudy or Aerosol-laden Conditions Xin Xi April 1, 2008.
A detailed look at the MOD16 ET algorithm Natalie Schultz Heat budget group meeting 7/11/13.
Scott Goetz Changes in Productivity with Climate Change at High Latitudes: the role of Disturbance.
Field Measurements of Leaf Mass Area (LMA) in Support of Remote Sensing Studies of a Pacific Northwest Old Growth Forest Canopy Katie Berger (UMASS-Amherst)
Next week’s assignment: 1) Using clumping indexes, LAI and  values for a conifer stand (Loblolly pine forest, Duke Univ.) and for a Eucalyptus plantation.
Predicting climate change impacts on southern pines productivity in SE United States using physiological process based model 3-PG Carlos A. Gonzalez-Benecke.
Extension of the forest ecosystem simulation model FORECAST: incorporating mountain pine beetle, fire, climate change, and wildlife Hamish Kimmins, Kim.
Introduction 1. Climate – Variations in temperature and precipitation are now predictable with a reasonable accuracy with lead times of up to a year (
Application of the ORCHIDEE global vegetation model to evaluate biomass and soil carbon stocks of Qinghai-Tibetan grasslands Tan Kun.
Modelling Crop Development and Growth in CropSyst
Disturbance Effects on Carbon Dynamics in Amazon Forest: A Synthesis from Individual Trees to Landscapes Workshop 1 – Tulane University, New Orleans, Late.
Variations in Continental Terrestrial Primary Production, Evapotranspiration and Disturbance Faith Ann Heinsch, Maosheng Zhao, Qiaozhen Mu, David Mildrexler,
Predicting Current and Future Tree Diversity in the Pacific Northwest I R S S Richard Waring 1 Nicholas Coops 2 1 Oregon State University 2 University.
Goal: to understand carbon dynamics in montane forest regions by developing new methods for estimating carbon exchange at local to regional scales. Activities:
1 Hadley Centre for Climate Prediction and Research Vegetation dynamics in simulations of radiatively-forced climate change Richard A. Betts, Chris D.
Predicting current and future tree diversity in the Pacific Northwest I R S S Richard Waring 1 & Nicholas Coops 2 1 Oregon State University 2 University.
Spring Budburst Study A Research project Model Secondary School for the Deaf Indiana School for the Deaf Spring 2007.
Remote-sensing and biodiversity in a changing climate Catherine Graham SUNY-Stony Brook Robert Hijmans, UC-Berkeley Lianrong Zhai, SUNY-Stony Brook Sassan.
Adaptation of forest operations to a changing climate Dr. Georgios Xenakis and Duncan Ray Ecology Division Forest Research, Northern Research Station,
Radial growth in Pinus contorta relative to changing climate patterns in British Columbia: Genetic response to annual climate variations, Sierra.
Figure 1. (A) Evapotranspiration (ET) in the equatorial Santarém forest: observed (mean ± SD across years of eddy fluxes, K67 site, blue shaded.
Understanding Site-Specific Factors Affecting the Nutrient Demands and Response to Fertilizer by Douglas-fir Center for Advanced Forestry Systems 2010.
Climate Change and Agricultural: Trends and Bi-Directional Impacts Dennis Baldocchi Department of Environmental Science, Policy and Management University.
Airborne LiDAR requires purchase, but offers a number of advantages; Airborne LiDAR requires purchase, but offers a number of advantages; Spatial resolution.
Center for Advanced Forestry Systems 2014 Meeting Do Below Ground Processes Explain Differences in Growth, Productivity and Carrying Capacity of Loblolly.
Figure 10. Improvement in landscape resolution that the new 250-meter MODIS (Moderate Resolution Imaging Spectroradiometer) measurement of gross primary.
and Other Related Measurements
Using vegetation indices (NDVI) to study vegetation
Upper Rio Grande R Basin
Chapter 5 Stand Dynamics & Gap Models
ln(CR) = HAB + b1BA + b2BA2 + b3ln(BA)
Western Mensurationists Meeting 2016
3-PG The Use of Physiological Principles in Predicting Forest Growth
Figure 1. Comparisons across evergreen coniferous (green bars), deciduous broadleaf (blue bars) and tropical forests (red bars), regarding (A) NEP in proportion.
KLAUS KDA1 – Biomass Estimation
Effects of Temperature and Precipitation Variability on Snowpack Trends in the Western U.S. JISAO/SMA Climate Impacts Group and the Department of Civil.
Sources of Variability in Canopy Spectra and the Convergent Properties of Plants Funding From: S.V. Ollinger, L. Lepine, H. Wicklein, F. Sullivan, M. Day.
Fig. 2 Absolute recovery of species richness and relative recovery of species richness and composition in relation to stand age for Neotropical secondary.
Big data for Global Change Ecology (Biogeography)
The effects of Canopy Cover on Herbaceous Vegetation
Presentation transcript:

Assessing the occurrence, vulnerability, expansion and disturbance of forests of the Pacific Northwest in response to recent climate variation Nicholas Coops Canadian Research Chair in Remote Sensing Department of Forest Resource Management Forest Sciences Centre. 2424 Main Mall. University of British Columbia. And Richard H Waring Oregon State University

Context In the Pacific northwestern (PNW) region of North America, climatic conditions have significantly warmed since a predominantly cool phase of the Pacific North American circulation patterns between 1950-1975.

What are the implications of this shift in climate for the vulnerability of native tree species? In places where species are predicted to have been less well suited, is there evidence of increased disturbance as assessed by remote sensing ?

Hybrid Modeling Approach Use a physiological model (3-PG) to predict how photosynthesis and canopy leaf area on Douglas-fir respond to climate change (1950-1975) versus (1976-2006) Define competitive climatic niches of other tree species in reference to physiological thresholds expressed for Douglas-fir Use the MODIS Disturbance index to link predicted tree species stress to observed disturbance

Phase I: The 3PG Model Freely downloadable in Excel format (developed by Peter Sands) C++ version which reads spatial data files (raster coverages) also freely available Developed by Landsberg and Waring (1997)

3PG Landsberg and Waring 1997 GPP NPP Absorption Utilization Photosynthetically Active Radiation (PAR) GPP x Fractional Interception x Physiological modifiers (Avg Tree Age, ASW, VPD, temperature) x Frost modifier x Temperature modifier x Quantum Efficiency = ƒ (Nutrient modifier) x Ratio NPP to GPP Rainfall Available Soil Water Transpiration Evaporation Fraction of NPP Fraction of NPP to Stem Root matter Foliage Turnover NPP Standing Volume Stem x Foliage allometrics x Stem allometrics Absorption Photosynthesis Utilization Respiration The partitioning fraction depends on Tree Age, ASW, VDP and fertility Landsberg and Waring 1997

Use of Modifiers Like other models 3PG makes use of modifiers which are dimensionless values, varying between zero (shut down) and unity (optimum). They represent the degree to which photosynthesis is limited by (a) water, (b) atmospheric vapour pressure deficits (c) suboptimal temperatures, and (d) frost damage. 1: Full Growth 0: No Growth 7

Environmental constraints on photosynthesis for Douglas-fir vary seasonally in the Pacific NW, U.S.A. soil water evaporative demand suboptimal temperature Frost limitations Autumn Summer Winter Spring

The 3-PG Model has been well calibrated for Douglas-fir Waring RH, N McDowell 2002 Use of a physiological process model with forestry yield tables to set limits on annual carbon balances. Tree Physiology 22:179-188 Swenson JJ, RH Waring, W Fan, NC Coops 2005 Predicting site index with a physiologically based growth model across Oregon, USA. Canadian Journal of Forest Research 35:1697-1707 Coops NC, SB Coggins, WA Kurz 2007 Mapping the environmental limitations to growth of coastal Douglas-fir stands on Vancouver Island, British Columbia. Tree Physiology 27:805-815

Data for 3PG: CLIMATE WNA Easy to use interface. Suite of climate layers and climate change scenarios Can generate point files or GIS layers of climate http://www.genetics.forestry.ubc.ca/cfcg/ClimateWNA/ClimateWNA.html

Soil Data To limit the analysis to climatic effects, we set the available water holding capacity at 200 mm for a sandy loam soil throughout the region. We also assigned a constant soil fertility rank of 50% of maximum, which results in an even partitioning of growth above- and belowground

Species Databases For British Columbia, tree species were taken from polygons located in protected forested areas and from vegetation resource inventory plots Accuracy of plot coordinates is roughly ± 500 m. For the United States, tree species data were taken from USFS Forest Inventory and Analysis plots. FIA data are recorded on a permanent sampling grid established across the conterminous United States at a density of approximately one plot per 2,400 ha As actual FIA plot locations are confidential, we used the publically available coordinates which have similar spatial accuracy as the Canadian data (i.e., ± 500 m). The presence / absence data from both Canada and the US were combined into one database with a total of 22,771 plots.

Plot Locations

3-PG Predicted Modifiers

3-PG Predicted Modifiers

Phase II of the modelling Define competitive climatic niches of other tree species in reference to physiological modifers expressed for Douglas-fir

We applied the 3-PG model to predict stand growth / LAI @ 50 yr using 1950–75 average climate. The model was then stopped and at 22,771 plots, monthly climatically-restricting modifiers were extracted. Decision tree analysis applied to develop models. A confusion matrix was developed which provides an indication of the positive and negative predictive power was well as kappa statistic We also used existing USFS maps of species’ distributions (Little 1971, esp.cr.usgs.gov/data/atlas/little/)

Decision tree analysis for LPP [Values in reference to optimum for Douglas-fir] After Coops & Waring. 2010. Climatic Change.

Douglas-fir

Lodgepole Pine

Translating Distribution Models to Stress-Based Information Use the decision tree model developed for each species using the long term (1950-75) climate Apply the model each year to the monthly climate data from 1976 – 2006 Years which have climate which correspond to the long term climate will be well suited to the species and thus we assume no stress Years which have climate outside the modelled range for the species will be years the species is “stressed” We then “count” the number of stressed years

(1976 - 2006)

Predicted stressed (red) and improved areas (green) since 1950-75 period

Phase III: Comparison against MODIS Disturbance Index Disturbance index utilizes a simple ratio of Annual-maximum composite LST and Annual-maximum EVI (greenness) to identify inter-annual changes in surface energy partitioning.   The DI is calculated on a per-pixel basis, and in this example, it is calculated annually.    +/-1 standard deviations away from the DI defines the range of natural annual variability.   SD above or below this indicates significant change in surface energy partitioning.  Above can indicate ‘negative’ disturbance (e.g. wildfire). Scores below 1 SD indicates areas of recovery.

Indicator: Disturbance Mildrexter et al (2007)

Indicator: Disturbance The disturbance index for 2000, 2003, and 2006. Areas of grey are indicative no change, bright red indicates major disturbance in 2000, Green indicates disturbance in 2003 and blue in 2006.

Predicted versus observed disturbance in Pacific NW Ecoregions Satellite-observed Disturbance (MODIS) EPA defined ecoregions Predicted stressed area (1990-2000)

Correlation between relative number of tree species stressed within an ecoregion vs. observed disturbance =0.7

Conclusions Hybrid approach has promise.. Partial validation: predicts reasonable values of max LAI, recorded distributions of 15 conifers, Stressed areas in ecoregions that correlate with the fraction of forested areas observed as recently disturbance Models appear to be accurate based on plot data New project underway to test model predictions with regeneration surveys in regions identified as stressed and recently disturbed Results are published in J. App. Veg. Science, Ecological Modeling and Remote Sensing of Environment.

All model outputs are available at: http://www.pnwspecieschange.info/ Project partly funded by a NASA Biodiversity and Ecological Forecasting Grant Collaborators: Steve Running David Mildrexler Maosheng Zhao University of Montana Clayton Beier Raphael Roy-Jauvin Tongli Wang University of British Columbia