| contributor author | McElroy, Michael B. | |
| contributor author | McConnell, John C. | |
| date accessioned | 2017-06-09T14:16:00Z | |
| date available | 2017-06-09T14:16:00Z | |
| date copyright | 1971/09/01 | |
| date issued | 1971 | |
| identifier issn | 0022-4928 | |
| identifier other | ams-16008.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4151744 | |
| description abstract | Detailed calculations are presented for the production of O and CO in the Martian atmosphere. The diffusion equations are solved and results compared with Mariner observations of O and CO in the upper Marian atmosphere. An eddy diffusion coefficient of 5 ? 108 cm2 sec?1 is required to account for these observations. Transport alone cannot explain the small abundances of CO and O2 in the lower atmosphere of Mars and chemical schemes suggested earlier encounter various difficulties. | |
| publisher | American Meteorological Society | |
| title | Dissociation of CO2 in the Martian Atmosphere | |
| type | Journal Paper | |
| journal volume | 28 | |
| journal issue | 6 | |
| journal title | Journal of the Atmospheric Sciences | |
| identifier doi | 10.1175/1520-0469(1971)028<0879:DOCITM>2.0.CO;2 | |
| journal fristpage | 879 | |
| journal lastpage | 884 | |
| tree | Journal of the Atmospheric Sciences:;1971:;Volume( 028 ):;issue: 006 | |
| contenttype | Fulltext | |