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Climate

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Carbon Cycle: Key Ideas. ... Plankton use dissoved CO2 in water for photosynthesis. ... Increased use of solar energy or wind power. – PowerPoint PPT presentation

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Title: Climate


1
Climate the Carbon Cycle
  • Earth is a closed system. Carbon is not gained
    or lost, it just cycles through the different
    spheres (Atmosphere Hydrosphere Geosphere
    Biosphere)
  • Atmospheric CO2 is a GHG. It traps I.R. energy
    radiated from Earths surface temperatures
    increase.

2
Climate Change Global Warming
  • Global Warming Increase in air and ocean
    temperatures.
  • Due to changes in Earths Energy Budget.

3
Greenhouse Effect CO2
  • Greenhouse Gases Gases that prevent I.R.
    wavelengths from Es surface from escaping to
    outer space.
  • CO2 GHG

4
Measuring Carbon Dioxide in the Atmosphere
  • Ice Cores Gas bubbles trapped in ice are
    miniature atmospheres that can be studied.
  • Measured directly from. Mauna Loa

5
Carbon Dioxide Levels
  • CO2 levels are determined from gas bubbles
    trapped in ice (Vostock Lake, Antarctica)
  • Temperatures can be determined from 18O16O
    ratios.

6
  • CO2 levels are determined from gas bubbles
    trapped in ice (Vostock Lake, Antarctica)
  • Temperatures can be determined from 18O16O
    ratios.

7
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8
Evidence of Global Warming Measured increases
in Carbon Dioxide Levels
  • Modern CO2 levels measured at Mauna Loa
    Observatory, Hawaii

9
Evidence of Global Warming Increasing Sea
Surface Temperatures Sea Level Rise
10
Evidence of Global Warming Glacial Retreats
11
Carbon Cycle Key Ideas Reservoirs a term used
to describe the compartments that contain carbon
in some form (e.g. atmosphere, soil, water, in
plants, etc) Photosynthesis CO2 from atmosphere
turned into sugar Respiration cells convert
sugars from food into CO2 Fossilization
processes involving extreme pressures that turn
various kinds of carbon into fossil fuels (coal,
crude oil, natural gas) Sedimentation material
settles to bottom of aquatic system Food Chain
carbon is transferred up the food chain as
animals consume plants and other animals.
Eventually, upon death, the carbon is returned to
soil and sediments. Volcanism volcanoes can
cycle carbon back to the atmosphere. As rock
melts to form magma, carbonate (CO3-2) is turned
into CO2 Chemical Weathering Carbon dioxide
from air dissolves in water to form carbonic
acid. Carbonic acid weathers rock
surfaces. Combustion fires or burning of fossil
fuels returns carbon to the atmosphere
12
Atmospheric CO2
dissolving
CO2 Dissolved in Ocean
Carbon in Trees, Plants, Algae
Uplift Mt. Building exposes new rock
uptake
Carbonate (CaCO3) Rock (limestone)
Carbon in Fossil Fuels
Carbon in Animals
Carbonate (CaCO3) in shells, etc
Carbon in Sediment
Carbon in Soil
13
fires
dissolving
Atmospheric CO2
CO2 Dissolved in Ocean
photosynthesis
Chemical weathering
Respiration
burning
volcanoes
Carbon in Trees, Plants, Algae
Respiration
Uplift/Mt. Buidling exposes new rock
Carbon in Fossil Fuels
uptake
Food Chain
Bacterial Respiration
Carbonate (CaCO3) Rock (limestone)
Carbon in Animals
fossilization
pressure
Carbonate (CaCO3) in shells, etc
Carbon in Sediment
Carbon in Soil
14
Geosphere ? ? Atmosphere
  • Volcanism ADDS CO2 to the atmosphere.
  • Mt. Building the chemical weathering of new
    rock REMOVES CO2 from the atmosphere.

15
Geosphere ? ? Atmosphere
16
Atmosphere ? ? Hydrosphere ? Geosphere
Plankton settle to bottom of ocean floor.
Sediment layers become rock.
Dissolved CO2 used by plankton which die
CO2 gas
17
Biosphere ? Geosphere
  • Plankton use dissoved CO2 in water for
    photosynthesis.
  • Plankton die (or are consumed/decomposed by other
    organisms, which die).
  • Dead plankton bring carbon to the ocean floor
    where it will become ROCK.

18
Warming or Cooling?
  • Increased volcanism?
  • Increase in mountain building weathering?
  • Deforestation?
  • Increased photosynthesis by marine plankton?
  • Increased frequency of forest fires?
  • Increased combustion of fossil fuels?
  • Decreased volcanic activity
  • Increased use of solar energy or wind power.

19
Ways to Reduce atmospheric CO2?
  • Reduced volcanism?
  • Mountain building increased weathering?
  • Increased photosynthesis?
  • Increased absorption of CO2 by ocean?
  • Changing land use (forests, urban areas, etc.)?
  • Increase the amount or rate that carbon becomes
    rock?
  • Decrease combustion of fossil fuels?

20
Results of increased levels of CO2
  • Increased atmospheric and sea surface
    temperature.
  • Ice caps/glaciers melt.
  • Flooding of coastal areas due to sea level rise.
  • Droughts in some locations/increased productivity
    in others.
  • Decrease in salinity of ocean water changes ocean
    circulation ( climate patterns).
  • Ocean acidification (dissolved CO2 forms an acid
    in water) ? reef organisms dissolve
  • Increase in insect borne (tropical) diseases
    (Malaria, etc.)
  • Economic loses.

21
  • Results of Global Warming
  • Flooding due to rise in sea level.
  • Change in who grows food.
  • Coral reefs die b/c acidification.

22
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