16
The Green House Effect ISCI 2001

The Green House Effect ISCI 2001. (1). The fate of solar radiation 26% reflected back into space 20% clouds; 6% by atmosphere 19% absorbed by clouds,

Embed Size (px)

DESCRIPTION

(1). Short-wave radiation from Sun – As it hits the surface converted into sensible heat Heats ground and lower atmosphere (2). Surface Radiation (infrared radiation) – Directed back into space as long-wave radiation – 90% absorbed by ‘ greenhouse ’ gases CO 2 (main GH gas); O 3 ; water vapor; methane; N 2 O (3). Gases are ‘ warmed ’ and heat Earth’s atmosphere (1). Short-wave radiation from Sun – As it hits the surface converted into sensible heat Heats ground and lower atmosphere (2). Surface Radiation (infrared radiation) – Directed back into space as long-wave radiation – 90% absorbed by ‘ greenhouse ’ gases CO 2 (main GH gas); O 3 ; water vapor; methane; N 2 O (3). Gases are ‘ warmed ’ and heat Earth’s atmosphere

Citation preview

Page 1: The Green House Effect ISCI 2001. (1). The fate of solar radiation  26% reflected back into space 20% clouds; 6% by atmosphere  19% absorbed by clouds,

The Green House Effect

ISCI 2001

Page 2: The Green House Effect ISCI 2001. (1). The fate of solar radiation  26% reflected back into space 20% clouds; 6% by atmosphere  19% absorbed by clouds,

• (1). The fate of solar radiation– 26% reflected back into space• 20% clouds; 6% by atmosphere

– 19% absorbed by clouds, ozone gas (O3)

– 55% reaches surface• 4% reflected at surface; 51% absorbed by

surface

Page 3: The Green House Effect ISCI 2001. (1). The fate of solar radiation  26% reflected back into space 20% clouds; 6% by atmosphere  19% absorbed by clouds,

• (1). Short-wave radiation from Sun– As it hits the surface converted into

sensible heat• Heats ground and lower atmosphere

• (2). Surface Radiation (infrared radiation)– Directed back into space as long-wave

radiation– 90% absorbed by ‘greenhouse’ gases• CO2 (main GH gas); O3 ; water vapor;

methane; N2O

• (3). Gases are ‘warmed’ and heat Earth’s atmosphere

Page 4: The Green House Effect ISCI 2001. (1). The fate of solar radiation  26% reflected back into space 20% clouds; 6% by atmosphere  19% absorbed by clouds,

• (1). Gases absorb (trap) heat to warm up our atmosphere• Absorbing longwave radiation from the

surface

• (2). Without GH Effect• Ave. Global Temp = -15 C• With GH = 15 C

Page 5: The Green House Effect ISCI 2001. (1). The fate of solar radiation  26% reflected back into space 20% clouds; 6% by atmosphere  19% absorbed by clouds,
Page 6: The Green House Effect ISCI 2001. (1). The fate of solar radiation  26% reflected back into space 20% clouds; 6% by atmosphere  19% absorbed by clouds,
Page 7: The Green House Effect ISCI 2001. (1). The fate of solar radiation  26% reflected back into space 20% clouds; 6% by atmosphere  19% absorbed by clouds,

• (1). Carbon dioxide– Fossil fuels; deforestation; organic decay; forest fires

• (2). Ozone– Sunlight chemically reacts with O2 (natural)– Photochemical smog production

• (3). Methane– Wetlands; biomass burning; termites; organic decay

• (4). Chlorofluorocarbons– Refrigerants; aerosol spray propellants; cleaning solvents

• (5). Nitrous Oxide – Fertilizers; burning of fossil fuels; forests; grasslands

Page 8: The Green House Effect ISCI 2001. (1). The fate of solar radiation  26% reflected back into space 20% clouds; 6% by atmosphere  19% absorbed by clouds,

• (1). Rising levels – 1700’s (280 ppm) ------------- 2005 (380

ppm)

• (2). Causes of increased CO2

– Fossil fuel combustion (65% of increase)– Deforestation/ Natural habitats to

agricultural areas • Natural ecosystem hold 20-100 times more

CO2

Page 9: The Green House Effect ISCI 2001. (1). The fate of solar radiation  26% reflected back into space 20% clouds; 6% by atmosphere  19% absorbed by clouds,
Page 10: The Green House Effect ISCI 2001. (1). The fate of solar radiation  26% reflected back into space 20% clouds; 6% by atmosphere  19% absorbed by clouds,
Page 11: The Green House Effect ISCI 2001. (1). The fate of solar radiation  26% reflected back into space 20% clouds; 6% by atmosphere  19% absorbed by clouds,

• (1). Methane (CH4)– 150% increase in levels since 1750– See sources

• (2). CFC’s destroy Ozone– Freon; Sprays – Damage near the poles – UV light

Page 12: The Green House Effect ISCI 2001. (1). The fate of solar radiation  26% reflected back into space 20% clouds; 6% by atmosphere  19% absorbed by clouds,
Page 13: The Green House Effect ISCI 2001. (1). The fate of solar radiation  26% reflected back into space 20% clouds; 6% by atmosphere  19% absorbed by clouds,
Page 14: The Green House Effect ISCI 2001. (1). The fate of solar radiation  26% reflected back into space 20% clouds; 6% by atmosphere  19% absorbed by clouds,

• (1). Temperature and Clouds– As GH gases increase, temperature

increases– Causes more cloud formations– Clouds reflect more energy into space– Reduce the amount of energy absorbed

and retained in the atmosphere

• (2). Counters the GH effect?

Page 15: The Green House Effect ISCI 2001. (1). The fate of solar radiation  26% reflected back into space 20% clouds; 6% by atmosphere  19% absorbed by clouds,

• (1). National Academy of Science – Increase of 1 F in 20th century

• (2). Recent Data (National Geographic)– 1.4 F increase since 1880 – Last (2) decades hottest in 400 years – Arctic temperatures risen 2x average– Glacier Ntl. Park 27 glaciers• 150 in 1910

Page 16: The Green House Effect ISCI 2001. (1). The fate of solar radiation  26% reflected back into space 20% clouds; 6% by atmosphere  19% absorbed by clouds,

• (1). 2500 scientist/130 countries– Industry, deforestation, increased

greenhouse gases and pollution– Combustion and carbon dioxide

• (2). Natural climatic cycles?