| contributor author | Paluch, I. R. | |
| contributor author | McKeen, S. | |
| contributor author | Lenschow, D. H. | |
| contributor author | Schillawski, R. D. | |
| contributor author | Kok, G. L. | |
| date accessioned | 2017-06-09T14:33:20Z | |
| date available | 2017-06-09T14:33:20Z | |
| date copyright | 1995/08/01 | |
| date issued | 1995 | |
| identifier issn | 0022-4928 | |
| identifier other | ams-21554.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4157906 | |
| description abstract | A diurnally averaged ozone decay rate of about 0.11 day?1was observed under partly cloudy sky in the boundary layer over the eastern Atlantic during the second Lagrangian experiment in the Atlantic Stratocumulus Transition Experiment. The observed decay rate can be accounted for by the combined effects of ozone loss through photolysis by UV radiation, reaction With H02 radical, and deposition on the sea surface, and effects of ozone production through photooxidation of carbon monoxide and methane in the presence of nitrogen oxides. The main contributor to the ozone decay is photolysis by UV radiation, but the other sources and sinks also make significant contributions. | |
| publisher | American Meteorological Society | |
| title | Evolution of the Subtropical Marine Boundary Layer: Photochemical Ozone Loss | |
| type | Journal Paper | |
| journal volume | 52 | |
| journal issue | 16 | |
| journal title | Journal of the Atmospheric Sciences | |
| identifier doi | 10.1175/1520-0469(1995)052<2967:EOTSMB>2.0.CO;2 | |
| journal fristpage | 2967 | |
| journal lastpage | 2976 | |
| tree | Journal of the Atmospheric Sciences:;1995:;Volume( 052 ):;issue: 016 | |
| contenttype | Fulltext | |
