Title: Climate Change
1Climate Change Ecosystem Ecology
- Ecosystems as Energy Machines
In an ecosystem approach, we pay less attention
to individual organisms / species than to
system-wide properties
2- Ecosystems as Energy Machines
- Most energy enters ecosystems via sunlight
- Photoautotroph derives its energy from sunlight
- Heterotroph derives its energy from other
organisms - The energy can be measured as NPP, or g
carbon/m2/yr
3- Large-scale NPP can be estimated with satellites.
How? - Satellites measure near infrared (NIR) and red
(RED) reflectance from plants. - NIR light is actively reflected by plants b/c it
is too low-energy for photosynthesis. It just
heats up the plant. - RED light tends to be absorbed for
photosynthesis. - The ratio of NIR reflected to RED reflected is
called the normalized difference vegetation index
(NDVI) - NIR RED / NIR RED
- NDVI correlates with NPP
4- See Fig. 25.15 for land-based NDVI estimates.
5- Using conversions you dont need to know,
reflectance can be converted to NPP - (See text, pp. 527-529)
http//earthobservatory.nasa.gov/Newsroom/NPP/Imag
es/psn.modis.seasonal.jpg
6- Change in N. Am. NPP, 1982-1998
- Based on satellite measurements
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8- Over small areas, NPP (g carbon/m²/year ) can be
measured on the ground as - NPP ?B L G
- Where ?B biomass after biomass before
- L biomass lost by death of plants
- G biomass lost to herbivory
9- Biomass (grams dry weight) can be converted to
energy (calories) in a bomb calorimeter. - A simple calorimeter?
- Thermometer attached to an insulated container.
- Different plant parts need to be measured
separately. - Calorie energy needed to increase 1 g of water
by 1Â C. ( 4.185 Joules.)
10- Ecosystems as energy machines
- NPP can be converted to energy
- Sometimes this is done with fossil NPP
- e.g. coal, oil, natural gas
- Sometimes this is done with more recent NPP
- e.g. wood, biofuels
11- Trace all relevant impacts of biofuels on the
carbon cycle
Fossil fuels needed to produce the biofuel
Energy output / energy inputs Land use changes
needed to produce the biofuel See FA_Land
Clearing Biofuel Carbon Diet
12- What factors might limit NPP?
- Amount of light entering the system
-
- Biomass of primary producers
- Photosynthetic rates of primary producers
- Respiration rates of primary producers
- Growth rates of primary producers
- Nutrient limitation
13- NPP limitation in terrestrial ecosystems
- Rosensweig 1968 NPP correlated with?
- actual evapotranspiration
14Rosensweig 1968
15- Evapotranspiration (ET) - the sum of evaporation
and plant transpiration at a location. - Transpiration is the loss of water as vapor
through stomata. - Potential evapotranspiration (PET) indicates
the energy (solar radiation temperature)
available to evaporate water, and the wind
available to transport the water vapour into the
lower atmosphere. - Assumes moisture is unlimited
16Is this a dry or moist environment?
17Is this a dry or moist environment?
18How will changes in AET influence NPP globally?
Ecosystem-level question How will all components
of climate change interact to affect NPP (and
therefore carbon storage) globally?
19- Effects of climate on NPP are very hard to
predict due to variable, interacting factors - Global nitrogen levels are rising
- Precipiation rising in some places, falling
others - CO2 concentrations rising
- Simulated warming often increases decomposition
more than NPP
20- How can this be studied experimentally?
- See SH_CO2 decreases plant growth
- Sometimes, experiments serve to raise more
questions than they answer.