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Spatial variation in autumn leaf color Matt Hinckley EDTEP 586 Autumn 2003
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Preview Introduction Background Initial model Methods Results Data, maps, graph Discussion Evidence for claim Revision of model
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Introduction: background Leaves change color in the fall when they lose their chlorophyll Altitudinal succession mirrors latitudinal succession Does this principle hold true in this case? Trees “know” when it’s fall
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Introduction: background Leaves change color in the fall when they lose their chlorophyll Altitudinal succession mirrors latitudinal succession Does this principle hold true in this case? Trees “know” when it’s fall
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Introduction: background Leaves change color in the fall when they stop making chlorophyll Altitudinal succession mirrors latitudinal succession Does this principle hold true in this case? Trees “know” when it’s fall
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Introduction: background Leaves change color in the fall when they stop making chlorophyll Altitudinal succession mirrors latitudinal succession Does this principle hold true in this case? Trees “know” when it’s fall Factors: Light, temperature, precipitation
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Introduction: background Leaves change color in the fall when they stop making chlorophyll Altitudinal succession mirrors latitudinal succession Does this principle hold true in this case? Trees “know” when it’s fall Factors: Light, temperature, precipitation ?
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Introduction: background Leaves change color in the fall when they stop making chlorophyll Altitudinal succession mirrors latitudinal succession Does this principle hold true in this case? Trees “know” when it’s fall Factors: temperature Light, temperature, precipitation ?
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Introduction: background Leaves change color in the fall when they stop making chlorophyll Altitudinal succession mirrors latitudinal succession Does this principle hold true in this case? Trees “know” when it’s fall Factors: temperature Light, temperature, precipitation Definitely changes by altitude in the Cascades ?
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Introduction: initial model Leaf color When leaves fall off Spatial variability
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Introduction: initial model Leaf color When leaves fall off Spatial variability Temp. Precip. Correlation Causal
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Introduction: initial model Leaf color When leaves fall off Spatial variability ? Temp. Precip. Light Correlation Causal Adiabatic cooling
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Introduction: initial model Leaf color When leaves fall off Spatial variability ? Temp. Precip. Light Correlation Causal Elevation Adiabatic cooling
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Introduction: assumptions Trees across the sample area will have leaves that can be observed on them Most problematic assumption: high elevation deciduous trees had lost all leaves Conducting observations ≥ 1 week apart would be OK It was not – leaves change fast, so only one observation was conducted I would be able to control for tree species
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Methods Driving the Puget Sound area Digital photography Image analysis Quantification of color GIS analysis of quantitative data Mapping Spatial interpolation
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Methods Driving the Puget Sound area Digital photography Image analysis Quantification of color GIS analysis of quantitative data Mapping Spatial interpolation
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Study area – driving
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Digital photos
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Methods Driving the Puget Sound area Digital photography Digital photos
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Methods Driving the Puget Sound area Digital photography Digital photos
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Methods Driving the Puget Sound area Digital photography
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Methods Hue Driving the Puget Sound area Digital photography Image analysis Quantification of color GIS analysis of quantitative data Mapping Spatial interpolation
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Methods Driving the Puget Sound area Digital photography Image analysis Quantification of color GIS analysis of quantitative data Mapping Spatial interpolation
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Results The data
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Results The data How to interpret it?
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Results: mapping
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Leaf color and elevation
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Freezing level ?
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Spatial interpolation
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Data limitations Image analysis problems Differences in lighting Selecting a tree to sample in each picture Tree species loosely controlled Limited sample size Snapshot in time and on Earth Therefore, claims may not be widely applicable
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Final Claim Generally, leaf color hue decreases along the visible spectrum as elevation increases Shown by data Temperature drops as altitude increases Known principle, observable in Cascades Therefore, lower temperature = more intense leaf color
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Initial revised model Leaf color When leaves fall off Spatial variability ? Temp. Precip. Light Correlation Causal Elevation Adiabatic cooling
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Final model Leaf color When leaves fall off Temp. Precip. Light Correlation Causal Elevation Adiabatic cooling Latitude Other factors Hard to test locally More easily tested ?
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Conclusions Data shows: Lower temperature = more intense leaf color We know that: Altitudinal succession = latitudinal succession Remains unclear whether these two principles can be applied together on a larger scale Regional/local limitation Further research: road trip to Alaska Control for tree species!
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