Unit10 Deforestation

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    DEFORESTATIONDEFORESTATIONDesign by Joe Naumann

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    Unit XI. Deforestation and the role of forests

    in the climate system.

    A. History of forests

    Earth 4.6 byr

    Life >3 byr

    Multicellular Life 600 myr

    Plants on land 400 myr (green algae)

    Ferns, etc. 200 - 70 myrFlowering plants 100 myr

    (Angiosperrms)

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    Unit XI. Deforestation and the role of forests in

    the climate system.

    A. History of forests

    First land plants short..

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    Unit XI. Deforestation and the role of forests

    in the climate system.

    B. Forest types

    Boreal Forests (conifers)

    Temperate Forests

    (mixed deciduous hardwoods)

    Tropical Rainforests

    (conifers and hardwoods)

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    NPP: Net Primary Productivity

    What is the net annual production of organicmatter by a particular ecosystem,usually

    measured in the amount of Carbon fixed as

    organic matter.Net means the total fixed minus the total

    respired.

    gC/km2/yris the (net) grams of carbon fixed

    over each square kilometer in an average year.

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    Characteristics of Earths Forests

    Forest

    Type

    Where? Area

    (km2

    )Rainfall Soil

    NPP

    gC/km2/yr

    Biodiv-

    ersity

    Boreal

    Temperate

    Tropical

    Rainforest

    High N

    Latitudes(50-60 N)

    Mid-

    Latitude(30- 50)

    Low

    Latitude

    (0 - 30)

    12 M

    12 M

    17 M

    Low

    20-50

    cm/yr

    Moderate

    50 to 100

    cm/yr

    High

    2 to 10

    m/yr

    Immature, but

    abundant

    minerals yet

    to be released

    Rich, fertile,

    abundant

    nutrient

    reservesPoor, highly

    leached. Most

    nutrients

    recycles

    300 M

    500 M

    1000 M

    Low

    High

    Moderate

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    Unit XI. Deforestation and the role of forests in

    the climate system.

    B. Forest types

    Boreal Forests: slow growing, cold, 1/2

    year low light, shallow, immature, but

    mineral-rich soils. Low plant and animal

    diversity.

    Capable of sustained harvest, but low yield

    (slow growth)

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    Unit XI. Deforestation and the role of forests in

    the climate system.

    B. Forest types

    Temperature Forests: Mixed deciduous

    hardwoods and evergreens, fertile soils.

    Resistent to disturbance: if cleared, rapid

    recolonization.

    Sustained yield OK in most regions.

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    Unit XI. Deforestation and the role of forests in

    the climate system.

    B. Forest types

    Tropical Rainforest: Closed canopy, high

    rainfall. Most in Brazil (Amazonia),

    central West Africa (Congo, Zaire),

    Indonesia and Madigascar. Also Central

    America, Angola, Peru, Bolivia, India and

    scattered outliers.

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    Percentage

    area coveredby different

    ecosystems

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    NPP (gC/m2/yr)

    for differentecosystems

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    Percentage net

    NPP

    (gC/m2/yr) fordifferent

    ecosystems

    70%

    3%

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    Unit XI. Deforestation and the role of forests

    in the climate system.

    B. Forest types

    Tropical Rainforest are the lungs of the

    world. They inhale CO2

    and exhale O2

    through the process of photosynthesis.

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    Unit XI. Deforestation and the role of forests

    in the climate system.

    B. Forest types

    Tropical Rainforest: The risky bit..

    Soils: Ancient, little rock, highly leached

    (high rainfall), and few sources of new

    nutrients. Almost all nutrients are

    recycled.

    Incapable of sustained high harvest.

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    Unit XI. Deforestation and the role of forests

    in the climate system.C. Deforestation: why we should be

    concerned.

    Loss of biodiversity

    Global warming (burning releases CO2)

    Climate impacts

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    Unit XI. Deforestation and the role of forests

    in the climate system.

    D. The role of forests in the climate system.

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    How a geologist

    views a tree.Key

    variables:

    Leaf area index

    Rooting depth

    Water-holding

    capacity of the soil.

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    D. The role of forests in the climate system.

    Amazonia: Estimated that 50% of the rainfall

    over the Amazon Basin is recycled water.

    During a rainfall event, leaves intercept rainwater,

    and organic-rich soil absorbs rainfall. Leaf

    evaporation and transpiration returns water vaporto the atmosphere.

    Two effects:

    landward migration of rainfall water vapor fuels more storms

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    D. The role of forests in the climate system.

    Amazonian Paradox:

    Amazon rainforest requires heavy rainfall to

    exist, but half the rainfall is itself depedent on

    the rainforest being present.

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    D. The role of forests in the climate system.

    Examples:

    Two adjacent catchments. One clear cut,

    the other left forested. Stream runoff in the

    deforested catchment was 4 to 10 times theforested catchment. Rainfall similar in the

    two basins, so difference is decreased

    evapotranspiration.

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    Forested Deforested

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    D. The role of forests in the climate system.

    Examples:

    Ivory Coast: Replacement of rainforest by cropland

    over last 5 deacdes,; runoff increased 8-fold.

    Areas formerly suitable for cocoa now abandoneddue to lower rainfall, less humidity and more

    extreme summer temperatures.

    Similar example in India where rice production fell

    after rainforest removed.

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    D. The role of forests in the climate system.

    Examples: Ivory Coast, India

    Proving cause and effect is difficult, but first

    principles provides a reasonable mechanism

    to explain these observations.