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Climate Change and Vegetation Phenology

Climate Change and Vegetation Phenology

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Climate Change and Vegetation Phenology. Climate Change. In the Northeastern US mean annual temperature increased 0.7 ° C over 30 years (0.26 ° C per decade) Expected another 2-6 ° C over next century - PowerPoint PPT Presentation

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Page 1: Climate Change and  Vegetation Phenology

Climate Change and Vegetation Phenology

Page 2: Climate Change and  Vegetation Phenology

Climate Change

• In the Northeastern US mean annual temperature increased 0.7°C over 30 years (0.26° C per decade)

• Expected another 2-6°C over next century

(Ollinger, S.V. “Potenail effects of climate change and rising CO2 on ecosystem process in northeastern U.S. forests)

Page 3: Climate Change and  Vegetation Phenology

Why does it matter?• Impacts on plant

productivity• Competition between

plant species• Interaction with other

organisms• Food production• Shifts in agricultural• Pest and disease

control• Pollen forecasts

• Carbon balance of terrestrial ecosystems

• Feedback into atmosphere

• Water, energy exchange

• Timing of migrations and breeding

• other ideas?

Page 4: Climate Change and  Vegetation Phenology

Phenology is the science that measures the timing of life cycle events in all organisms

Plants tell a story about climate……

Listening to the story they tell year after year can tell us about climate change

Earlier Springs Later Falls

Page 5: Climate Change and  Vegetation Phenology

Plants provide an excellent context to understand changes in the environment

They are extremely sensitive to:

• temperature change• precipitation change• growing degree days

Page 6: Climate Change and  Vegetation Phenology

Phenology: A glimpse of ecosystem Impacts

Some potential effects:– Wildlife populations– Vegetation health– Species composition and

ranges– Water availability– Nutrient cycling and

decomposition– Carbon storage

Page 7: Climate Change and  Vegetation Phenology

Measuring Phenology

Field Observations Satellite Remote Sensing

Page 8: Climate Change and  Vegetation Phenology

IntensiveSites

Spatially Extensive Science Networks

Remote Sensing andSynoptic (wall-to-wall) DataDe

crea

sing

Spat

ial

Cove

rage

Incr

easin

g Pr

oces

s Kno

wled

ge

Data

Qua

lity

# of

Mea

sure

men

ts

How do scientists monitor vegetation phenology?

Spatially Extensive Volunteer & Education Networks

AmeriFlux NWS Coop NPS Inv. & Mon. State Ag. Exp. Sta.

Nature Preserves, Campuses

NASA USGS NOAA

Tier 1

Tier 2

Tier 3

Tier 4

George R. Kish U.S. Geological Survey

Field Based

Satellite Based

Page 9: Climate Change and  Vegetation Phenology

Measuring Phenology on the ground

Field Observations

Page 10: Climate Change and  Vegetation Phenology

Sandra Wilmot Tom Simmons

Timing of sugar maple leaf dropMonitored at Proctor Maple Research Center

Page 11: Climate Change and  Vegetation Phenology

Hemispherical Photography

Helps us “see” the canopy as a satellite might see it

Page 12: Climate Change and  Vegetation Phenology

Hemispherical Imagery• Scientists spend big bucks to purchase the

equipment and software necessary to link ground measurements with satellite imagery.

• Calculate canopy closure, transparency, leaf area index, vegetation indices, gap fraction, etc.

Page 13: Climate Change and  Vegetation Phenology

Measuring Phenology

Satellite Remote Sensing

Land surface phenologies in 2000 revealed by three AVHRR biweekly composites.” From USA National Phenology Network (USANPN)

Page 14: Climate Change and  Vegetation Phenology

How do you see phenology from space?

http://www.fao.org/docrep/003/T0446E/T0446E04.htm

• Chlorophyll, strongly absorbs visible light for photosynthesis. • Leaf cell structure reflects near-infrared light.• NDVI exploits these characteristics of

vegetation reflectance to quantify how much, how dense and how productive vegetation is.

Page 15: Climate Change and  Vegetation Phenology

Normalized Difference Vegetation IndexNDVI

•Negative values of NDVI correspond to water. •Values close to zero correspond to barren areas of rock, sand, or snow. •low, positive values represent shrub and grassland •high values indicate temperate and tropical rainforests.

Page 16: Climate Change and  Vegetation Phenology

Corn/Soy belt Central Illinois

Kirsten M. de Beurs, Ph.D.Virginia Tech University

Page 17: Climate Change and  Vegetation Phenology

Death Valley

Kirsten M. de Beurs, Ph.D.Virginia Tech University

What would this NDVI curve look like?

Page 18: Climate Change and  Vegetation Phenology

ForestSouthwest Virginia

Kirsten M. de Beurs, Ph.D.Virginia Tech University

What would this NDVI curve look like?

Page 19: Climate Change and  Vegetation Phenology

Tundra Northern Alaska

Kirsten M. de Beurs, Ph.D.Virginia Tech University

What would this NDVI curve look like?

Page 20: Climate Change and  Vegetation Phenology

NDVI for Phenological Dates

• http://www.seiswaves.com/cappelluti/docs/anims/leicester/

comparison of NDVI values for different dates

Page 21: Climate Change and  Vegetation Phenology

SOS

Start of Season

End of Season

Duration of Season

Rate

of

Gree

nup

Maximum NDVI

Time Integrated NDVI

Rate of Senescence

Plotting NDVIUse of NDVI to identify key phenological dates

Page 22: Climate Change and  Vegetation Phenology

How do you determine dates?

Use of NDVI thresholds to identify key phenological dates

http://phenology.cr.usgs.gov/methods_metrics.php

Start of the Season

Page 23: Climate Change and  Vegetation Phenology

0.5 of the Max:Min NDVI ratio to approximate the start and end of the

season

00.10.20.30.40.50.60.70.8

J F M A M J J A S O N D

Months

NDV

I

EOS

Common Thresholds

Kirsten M. de Beurs, Ph.D. Virginia Tech University

Page 24: Climate Change and  Vegetation Phenology

50% Threshold (Seasonal Mid-point)

(White et al., mean day = 124, May 4th)

Page 25: Climate Change and  Vegetation Phenology

Other key phenological dates

http://phenology.cr.usgs.gov/methods_metrics.php