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Climate Change

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Using conversions you don't need to know, reflectance can be converted to NPP ... Based on satellite measurements ... Ecosystem-level question ... – PowerPoint PPT presentation

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Title: Climate Change


1
Climate 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

7
(No Transcript)
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 1 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

14
Rosensweig 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


16
Is this a dry or moist environment?
17
Is this a dry or moist environment?
18
How 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.
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