作者: Xiu-De Ling , Julius London
DOI: 10.1175/1520-0469(1986)043<3122:TQBOOO>2.0.CO;2
关键词: Climatology 、 Atmospheric models 、 Atmospheric sciences 、 Oscillation 、 Ozone 、 Radiative transfer 、 Tropical cyclone 、 Atmospheric chemistry 、 Stratosphere 、 Quasi-biennial oscillation 、 Environmental science 、 Atmospheric Science
摘要: Abstract A one-dimensional model of the quasi-biennial oscillation (QBO) ozone in tropical middle stratosphere is derived based on assumed (observed) zonal wind QBO a coupled dynamic, radiative/ photochemical system. It found that vertical variation amplitude has two. maxima, one at 32 km and other 22 km, minimum 28 km. These are qualitative agreement with observations. In height interval 30–35 closely related to temperature dependent photochemistry variations out phase. Below where thermal transports important, oscillations phase but both am approximately 270° variation.