An interpretation for the interannual variations of the global distribution of total ozone

Computer Science

Scientific paper

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Annual Variations, Atmospheric Circulation, Atmospheric Composition, Atmospheric Temperature, Ozone, Lagrange Coordinates, Meridional Flow, Oscillations, Planetary Waves, Sea Surface Temperature, Temperature Distribution, Trace Elements

Scientific paper

The quasibiennial oscillation (QBO) and the four year oscillation (FYO) in total ozone are discussed. In order to understand these oscillations, a comprehensive view of the ozone and the stratospheric temperature is attempted. The standpoint here is to examine if these oscillations could be understood as a reflection of the general circulation changes in the stratosphere. The description of the circulation is based on the Lagrangian-mean point of view, although only a rough estimate is obtained. For the sake of simplicity, the ozone is assumed to be an inert tracer following the atmospheric motion.

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