contributor author | Ling, Xiu-De | |
contributor author | London, Julius | |
date accessioned | 2017-06-09T14:26:56Z | |
date available | 2017-06-09T14:26:56Z | |
date copyright | 1986/12/01 | |
date issued | 1986 | |
identifier issn | 0022-4928 | |
identifier other | ams-19430.pdf | |
identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4155546 | |
description abstract | A one-dimensional model of the quasi-biennial oscillation (QBO) of ozone in the tropical middle stratosphere is derived based on assumed (observed) zonal wind QBO in a coupled dynamic, radiative/ photochemical system. It is found that the derived vertical variation of the ozone QBO amplitude has two. maxima, one at 32 km and the other at 22 km, and a minimum at 28 km. These are in qualitative agreement with observations. In the height interval 30?35 km, the ozone QBO is closely related to temperature dependent photochemistry and the ozone and temperature variations are out of phase. Below 28 km, where vertical ozone and thermal transports are important, ozone and temperature oscillations are in phase but both am approximately 270° out of phase with the vertical wind variation. | |
publisher | American Meteorological Society | |
title | The Quasi-biennial Oscillation of Ozone in the Tropical Middle Stratosphere: A One-Dimensional Model | |
type | Journal Paper | |
journal volume | 43 | |
journal issue | 24 | |
journal title | Journal of the Atmospheric Sciences | |
identifier doi | 10.1175/1520-0469(1986)043<3122:TQBOOO>2.0.CO;2 | |
journal fristpage | 3122 | |
journal lastpage | 3137 | |
tree | Journal of the Atmospheric Sciences:;1986:;Volume( 043 ):;issue: 024 | |
contenttype | Fulltext | |