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Title: ClimateFVS Version 0'1: Description of Content and Example Outputs


1
  • Climate-FVS Version 0.1 Description of Content
    and Example Outputs
  • Nicholas L. Crookston
  • Gary Dixon, Jerry Rehfeldt and many more
  • Rocky Mountain Research Station Moscow
  • National Silviculture Workshop
  • June 15-19, 2009

2
Contents
  • Introduction
  • Climate change makes a difference
  • Modeling species climate-profiles
  • Future climate and species distributions
  • Elements of Climate-FVS
  • Three examples
  • Pros and cons regarding the modeling.
  • Next steps

3
Douglas-fir climate profile location
change (current to 2060)
4
Aspen climate profile location change (current to
2060)
5
Black Mesa Western Colorado
6
Modeling species climate-profiles
  • Build contemporary climate surfaces
  • Get predictions of climate for each FIA plot in
    the western United States.
  • Use Random Forest classification to build a
    predictive model of the species climate profile
    (climate-based species viability).
  • To map the profile predict the viability for
    each 1 km pixel in the Western United States.

7
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8
Douglas-fir contemporary climate
Mapped at 1 km2 grid
9
Future climate and species distributions
  • Build future climate surfaces using outputs from
    3 global circulation models (GCM), run using 2 or
    3 scenarios to form 7 futures.
  • Predict and map the species viability for the
    future climates.

10
GCM General circulation model
  • There are many, we used these three
  • CGCM3 Canadian Center of Climate Modeling and
    Analysis, SRES scenarios A1B, A2, B1
  • HADMC3 Met Office Hadley Centre (UK), SRES
    scenarios A2, B1
  • GFDLCM21 Geophysical Fluid Dynamics Laboratory
    (Princeton University, NOAA Research), SRES
    scenarios A2, B2

11
2090 GDFL
2000
12
2090 GDFL
2000
13
Douglas-fir climate profile location
change (current to 2060)
14
Details in Rehfeldt et al. 2006. Empirical
analysis of plant-climate relationships for the
western United States. Int. J. Plant Sci.
167(6)11231150.
http//forest.moscowfsl.wsu.edu/gems/Biogeography.
pdf
15
Elements of Climate-FVS
  • Architecture and input
  • Site carrying capacity
  • Species composition
  • Mortality
  • Establishment
  • Tree growth
  • Genetics
  • Site

16
Architecture and input
  • The architecture of FVS was not changed.
  • Existing outputs and management actions
  • Input climate and species viability scores for
    each stand and GCM/scenario combination.
  • These data will be available from an internet
    site. You need to supply the location and
    elevation of each stand.

17
Site carrying capacity
  • Measured as max BA or max SDI
  • FVS contains species max BA or SDI.
  • A viability-weighed average is computed for
    contemporary climate and future climate. A ratio
    of these is used to adjust the FVS-estimate of
    carrying capacity.
  • Conversion from forest to non-forest and visa
    versa is supported by this logic.

18
Species composition
  • Mortality rates increase when the viability score
    fall below 0.50.
  • Establishment
  • Triggered by low stocking.
  • Add the most viable species.
  • Add more trees per acre of the most viable
    species.

19
Tree growth Site
  • Site changes are modeled as a function of change
    in annual dryness index (ADI).
  • Proportional change future/current.
  • An increasing ADI results in corresponding growth
    reductions and visa versa.

20
Tree growth Genetics
  • Basic idea use common garden data to calibrate
    growth models as a function of climate transfer
    distance the difference in climate at the
    planting site and the seed source.

21
Laura Leites, University of Idaho
Douglas-fir height growth
22
Tree growth Genetics
  • The change in relative growth is used to adjust
    growth.
  • computed by replacing space with time in these
    models
  • the effects are strongest for genetic
    specialists.
  • We have preliminary models for Larch and
    Douglas-fir, they are used for all species based
    on a ranking of genetic specialization.

23
Three examples
24
First example Clearwater
  • 135 stands on the Clearwater National Forest
  • One hundred year simulation
  • Output total basal area and trees per acre by
    species
  • Eight results
  • Base FVS (use the modified model with
    contemporary climate fixed over time)
  • 7 GCM/SRES model/scenario combinations

25
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26
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27
Second example Black Mesa
  • Recall the talk introduction.
  • 214 stands on the Grand Mesa, Uncompahgre,
    Gunnison National Forest (Black Mesa)

28
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29
Third example West Cascades
  • 310 stands on the Gifford Pinchot National Forest
  • For this area a additional element is include
    that represents change in growth depending on
    transfer distance, measured on climatic scales.

30
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31
Differences between examples
  • Impact differs between locations
  • Black Mesa IPCC A2 scenarios from the Canadian
    and GFDL models exhibit greatest impact.
  • Clearwater Hadley model for A2 and B2 scenarios
    exhibit the greatest impact.
  • West Cascades Low impact (but maybe false!).

32
Reasons for using the approach
  • Based on direct observations of the relationship
    between climate and species distributions
  • It places reasonable bounds on the spatial
    distribution of species
  • It is a consistent method over all species and
    regions

33
Proscontinued
  • Provides a framework for modeling what happens to
    forests when mature trees die and are replaced by
    small trees.
  • We can start to understand the scale of the
    variance between GCMs and IPCC scenarios.

34
Problems with the approach
  • For genetic specialists, (such as Douglas-fir and
    lodgepole), the method likely underestimates the
    effect climate change will have on mortality
    rates of existing trees.
  • Species migration rates are not represented.
  • The effect of climate change on growth rates
    (site index) is represented using the results of
    a limited analysis.

35
Cons continued
  • Physiological processes are not directly
    represented. We have tried 3PG to model changes
    in carrying capacity.
  • The climate model down-scaling does not represent
    fine-scale topographical elements that control
    micro climate.

36
Cons continued
  • Mortality will likely be caused by fire, insects,
    diseases, or these in combination. These
    simulations do not represent these episodic
    mortality causes, but they do, perhaps, represent
    the net effects of these events.
  • Many more!

37
Next steps
  • Get this model in your hands for testing,
    evaluation, and feed back.
  • Contact me or Dave Cawrse if you want to be a
    tester, ask questions, or make comments.
  • dcawrse_at_fs.fed.us
  • ncrookston_at_fs.fed.us

38
Acknowledgements
  • Funded by USFS Global Climate Change Research
    Program and the Rocky Mountain Research Station.
  • Many people who attended workshops where ideas
    were openly discussed Aaron Weiskittel,
    Abdel-Azim Zumrawi, Albert Stage, Ann Abbot, Bill
    Wykoff, Bob Monserud, Brad StClair, Bryce
    Richardson, Colin Daniel, Dave Cawrse, Dave
    Marshall, David Loftis, Dennis Ferguson, Don
    Robinson, Doug Berglund, Doug Maguire, Erin
    Smith-Mateja, Fred Martin, Glenn Howe, John
    Goodburn, John Marshall, Kelsey Milner, Laura
    Leites, Linda Joyce, Mee-Sook Kim, Megan
    Roessing, Mike Bevers, Mike Ryan, Peter Gould,
    Phil Radtke, Robert Froese, and Stephanie Rebain.
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