Earths Atmosphere Evolution Additional references Evolution of the

  • Slides: 27
Download presentation
Earth’s Atmosphere Evolution – Additional references – – – Evolution of the atmosphere (Walker,

Earth’s Atmosphere Evolution – Additional references – – – Evolution of the atmosphere (Walker, 1975) Chemistry of Atmospheres (Wayne, 1991) Chemistry of the Natural Atmosphere (Warneck, 2000) Kump, Nature, 2008 Falkowski, Science, 2005 Arrhenius law • Atmospheric fraction of CO 2 • Temperature structure – Manabe and Wetherald, JAS, 1967 – Manabe and Stickler, JAS, 1964 • Atmospheric radiation

Wayne, 1991 Warneck, 2000

Wayne, 1991 Warneck, 2000

Banded iron formations Red beds

Banded iron formations Red beds

Mass dependent fractionation Mass independent fractionation Kump, 2008

Mass dependent fractionation Mass independent fractionation Kump, 2008

Warneck, 2000

Warneck, 2000

Methanogens

Methanogens

http: //www. snowballearth. org/overview. html

http: //www. snowballearth. org/overview. html

Falkowski et al. , 2005

Falkowski et al. , 2005

Falkowski et al. , 2005

Falkowski et al. , 2005

KH Temperature (K)

KH Temperature (K)

JAS, 1964

JAS, 1964

Fraunhoffer Lines Fe Na O 2 H – Balmer series • First observed by

Fraunhoffer Lines Fe Na O 2 H – Balmer series • First observed by Wollatson (1802). Fraunhoffer independently discovered them in 1814 and studied them thoroughly. • The continuous emission of photosphere is interrupted by selective absorption and re-emission in upper photosphere. Seen in visible and IR spectra only as absorption lines. Lines at < 185 nm appear in emission. • Fraunhoffer mapped over 570 lines. Later these lines were associated with atoms/molecules in the upper solar atmosphere.

Primary atmospheric molecules involved in absorption of radiation • Atmospheric molecules are characterized by

Primary atmospheric molecules involved in absorption of radiation • Atmospheric molecules are characterized by discrete rotational and vibrational energy states in addition to the electronic transitions. • Transitions – Electronic – Ionization, dissassociation – UV some visible. – Vibrational – IR, far IR – Rotational – far IR, microwave • The lower energy states significantly impact terrestrial radiation, which peaks in the IR. Bohren and Clothiaux, 2006

Ionize Dissasociate Vibrational --- Rotational

Ionize Dissasociate Vibrational --- Rotational

CO 2 O 3 CH 4 H 2 O

CO 2 O 3 CH 4 H 2 O