Casey McCabe
Global Change: Biome Perspective
(Illustration by Nicolle Rager Fuller, National Science Foundation.)
Carbon sink through primary
production
Stores less than boreal and tropical
51% in living biomass
37% in dead wood, litter and soil
(Bonan 2008, Pan et al. 2011)
Important for regional carbon
budgets
Contribution to global water
cycle and cloud formation
Rates vary across forest types
Forests and crops have higher
evaporative cooling than
grasslands
Forests have l0w albedo
compared to grassland/crops
Land use change in past
converted large amount of
temperate forest to cropland
Highly managed
(Bonan 2008, Jackson et al. 2008, Peters et al. 2013)
Physicochemical
Changes
Indirect Effects
& Feedbacks
Megadisturbance
(Pautasso et al. 2012)
2013 IPCC Report
Temperature
Precipitation
CO2
Increased evaporation
Biological effects
Changes in phenology
Range shifts
Increased rain vs. snow and
snow melt
Heat stress
Changes in growth rate
▪ Increases and decreases
(van Mantgem 2009,
Keenan et al. 2014)
Very variable according to region
Increases in eastern U.S., northern Europe, southeast Asia
Decreases in western U.S., southern Europe, northeast
Asia, and eastern Australia
Some areas with increased drought or flooding
Flooding can increase or reduce nutrient levels
Drought can cause tree death and increase susceptibility to
pests, pathogens, and fire
(2013 IPCC Report, Bentz et al. 2010, Millar and Stephenson 2015)
Atmospheric CO2 is increasing
Positive for plant growth and water-use efficiency
▪ Response may be limited by water and nutrients
2013 IPCC Report
(Silva and Anand 2013)
(Bonan 2008)
Temp = Evaporation = Evaporative Cooling
Transpiration
Drought
Temp = Snow = Yearly Soil Moisture
CO2 = Transpiration = Drought Tolerance
Temp = Photosynthesis = Carbon Sink
CO2 = Photosynthesis = Carbon Sink
Water = Photosynthesis = Carbon Sink
(Keenan et al. 2014)
(Millar and Stephenson 2015)
(van Mantgem et al. 2009)
Baseline mortality of trees is
increasing
Dead trees release large
amounts of carbon
Old-growth forests store
more carbon
Overall, increase in large disturbances across
the globe related to global change forcings
More intense droughts, fires, biotic
outbreaks, and heat waves
(Dale et al. 2001, Millar and Stephenson 2015)
Increasing due to temperature increase
20.4 million hectares of forest in the US
impacted by biotic forcing (10 Massachusetts)
annually
The most expensive disturbances for humans
Magnitude of disturbance can equal or
surpass that of direct climate forcings
( Bentz et al. 2010)
(Flower and Gonzalez-Meler 2015)
Bentz, B. J. et al. Climate change and bark beetles of the western United States and Canada: Direct and indirect effects. Bioscience 60,
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Biol. 1–23 (2015).
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