Global Carbon Cycle 3/12 Carbon is exchanged between the active pools due to various processes – photosynthesis and respiration between the land and the.

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Presentation transcript:

Global Carbon Cycle 3/12 Carbon is exchanged between the active pools due to various processes – photosynthesis and respiration between the land and the atmosphere, and diffusion between the ocean and the atmosphere.

Carbon Pools 2/12 Carbon is stored on our planet in the following major pools: as organic molecules in living and dead organisms found in the biosphere; as the gas carbon dioxide in the atmosphere; as organic matter in soils; in the lithosphere as fossil fuels and sedimentary rock deposits such as limestone, dolomite and chalk; in the oceans as dissolved atmospheric carbon dioxide and as calcium carbonate shells in marine organisms.

Carbon (as CO 2 ) is accumulated… Carbon (as CO 2 ) is accumulated… – Photosynthesis uses sunlight to make carbohydrate from CO2. Carbon (as CO 2 ) is released… Carbon (as CO 2 ) is released… – Respiration - carbon is oxidized for energy. – Combustion - carbon is burned – Weathering - rain (slightly acidic) weathers calcium carbonate rocks

Carbon Cycle Has Been In Balance for Millions of Years But in the last century CO 2 levels have been creeping up. Why?

Carbon Cycle Has Been In Balance for Millions of Years But in the last century CO 2 levels have been creeping up. Why? - (burning of fossil fuels).

Greenhouse gasses in the atmosphere act like the glass in a greenhouse or car.

The Greenhouse Effect Think of the inside of a car in the summer… UV radiation from the sun passes through the glass, warms up the seats, and gets trapped Heat (infrared) doesn ’ t pass back out through glass easily

The Greenhouse Effect is a Good Thing Because Mars has almost no greenhouse gasses, heat from the sun goes back into outer space. Average temperature = -10 °F

Venus has too much of a good thing… High CO 2 levels on Venus trap too much heat. Temperature is nearly 800 °F. Even hotter than planet Mercury (350 °F), which is closer to the sun.

Atmospheric CO 2 Concentration-1 4/12 Accurate and direct measurements of the concentration of CO 2 in the atmosphere began in 1957 at the South Pole and in 1958 at Mauna Loa, Hawaii.

Atmospheric CO 2 Concentration-2 5/12 In 1958, the concentration of CO 2 was about 315 ppmv, and the growth rate was about 0.6 ppmv/yr. This growth rate has generally been increasing since then; it averaged 0.83 ppmv/yr in the 1960s, 1.28 ppmv/yr during the 1970s, and 1.53 ppmv/yr during the 1980s. The concentration in 2006 was over 380 ppmv. The annual cycle in the Mauna Loa record is due to the seasonality of vegetation. In early spring, the concentration of CO 2 is at its maximum, and as the plants green-up, the concentration drops, reaching a minimum value towards the end of the summer, and when leaves fall, it starts to build up again. This swing in the amplitude is most pronounced in the records from the northern high latitudes, where it can be as large as 15 ppmv.

Major Greenhouse Gasses Water vapor Water vapor Does much to keep planet warm. We have no control over water vapor. CO 2 CO 2 is the most significant greenhouse gas. Levels increasing because of fossil fuel burning. We should be concerned about this one.

Other Greenhouse Gasses Methane Methane - from wetlands, ruminants and commercial production times more potent than CO 2. Levels going up slowly. Nitrogen oxides (NO x or N x O) Nitrogen oxides (NO x or N x O) - formed during combustion from N 2 that ’ s in air times more potent than CO 2. Chloroflurocarbons (CFC ’ s) Chloroflurocarbons (CFC ’ s) - Foam insulation, refrigeration gas, used to be an aerosol propellant. Being phased out. Ozone Ozone - formed from lightning, electrical arcs, and a reaction of gas vapors and sunlight.