CO2 condensation and the climate of early Mars

Icarus

Volumn 94, Issue 1, 1991, Pages 1-13

  Kasting, James F ^a  

^a PENNSYLVANIA STATE UNIVERSITY   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

CARBON DIOXIDE; WATER;

ARTICLE; ASTRONOMY; ATMOSPHERE; CHEMICAL MODEL; CLIMATE; GREENHOUSE EFFECT; MICROCLIMATE; NASA DISCIPLINE EXOBIOLOGY; NASA DISCIPLINE NUMBER 52-30; NASA PROGRAM EXOBIOLOGY; NON-NASA CENTER; TEMPERATURE;

NASA DISCIPLINE EXOBIOLOGY; NASA DISCIPLINE NUMBER 52-30; NASA PROGRAM EXOBIOLOGY; NON-NASA CENTER;

ATMOSPHERE; CARBON DIOXIDE; CLIMATE; EXTRATERRESTRIAL ENVIRONMENT; GREENHOUSE EFFECT; MARS; MODELS, CHEMICAL; SOLAR SYSTEM; SUPPORT, U.S. GOV'T, NON-P.H.S.; TEMPERATURE; WATER;

EID: 0026412262     PISSN: 00191035     EISSN: 10902643     Source Type: Journal    
DOI: 10.1016/0019-1035(91)90137-I     Document Type: Article

References (60)

1. The vapour pressures and critical temperatures of acetylene and carbon dioxide
2. The Spokane flood controversy and the Martian outflow channels
3. 0 and the case of the missing lithium
4. 2
5. Stability of streams and lakes on Mars
6. The Martian paleoclimate and enhanced carbon dioxide
7. Thermodynamic properties of aqueous gas mixtures at advanced pressures
8. Simple strategies for inclusion of Voigt effects in infrared cooling rate calculations
9. Atmospheric pressure variation and the climate of Mars
10. Solar evolution
11. Ancient aqueous sedimentation on Mars
12. Solar interior structure and luminosity variations
13. Fluvial valleys and Martian paleoclimates
14. 2O atmospheres
15. Igneous fluids
16. Stellar evolution within and off the main sequence
17. The runaway greenhouse A history of water on Venus
18. Long-term stability of the Earth's climate
19. Runaway and moist greenhouse atmospheres and the evolution of Earth and Venus
20. 2 levels in the Earth's early atmosphere
21. Response of Earth's atmosphere to increases in solar flux and implications for loss of water from Venus
22. 2 levels on surface temperature and atmospheric oxidation state of the early earth
23. How climate evolved on the terrestrial planets
24. Thermal and albedo mapping of Mars during the Viking primary mission
25. A study of the radiative effects of enhanced atmospheric CO2 and CH4 on early earth surface temperatures
26. Ammonia photolysis and the greenhouse effect in the primordial atmosphere of the Earth
27. The effects of increased CO2 concentrations on surface temperature of the early earth
28. The role of convective model choice in calculating the climate impact of doubling atmospheric CO2
29. Thermal equilibrium of the atmosphere with a given distribution of relative humidity
30. The early environment and its evolution on Mars: Implications for life
31. Clathrate hydrates in the solar system
32. Carbon dioxide clathrate in the Martian ice cap
33. Early Earth An enhanced carbon dioxide greenhouse to compensate for reduced solar luminosity
34. Origin of Martian channels: Clathrates and water
35. Climatic change on the terrestrial planets
36. The case for a wet, warm climate on early Mars
37. 2) on Martian paleoclimate
38. The greenhouse theory of climate change: A test by an inadvertent global experiment
39. Infrared continuum absorption by atmospheric water vapor in the 8–12 μm window
40. Our sun. I. The standard model: successes and failures
41. Earth and Mars: Evolution of atmospheres and surface temperatures
42. The history of water on Mars
43. Atmospheric lapse rates and their parameterization
44. Rapid calculation of radiative heating rates and photodissociation rates in inhomogeneous multiple scattering atmospheres
45. The astronomical theory of climate change on Mars
46. Evolution of an impact-generated dust cloud and its effects on the atmosphere
47. Solar and terrestrial parameterizations for radiative-convective models
48. A negative feedback mechanism for the long-term stabilization of Earth's surface temperature
49. Evaporation of ice in planetary atmospheres: Ice-covered rivers on Mars
50. Optical constants of ice from the ultraviolet to the microwave
51. Optical constants of carbon dioxide ice
52. Mass loss on the main sequence
53. Primitive atmosphere and implications for the formation of channels on Mars