Hocke, K.; Sauvageat, E. Frequency Dependence of the Correlation between Ozone and Temperature Oscillations in the Middle Atmosphere. Atmosphere2023, 14, 1436.
Hocke, K.; Sauvageat, E. Frequency Dependence of the Correlation between Ozone and Temperature Oscillations in the Middle Atmosphere. Atmosphere 2023, 14, 1436.
Hocke, K.; Sauvageat, E. Frequency Dependence of the Correlation between Ozone and Temperature Oscillations in the Middle Atmosphere. Atmosphere2023, 14, 1436.
Hocke, K.; Sauvageat, E. Frequency Dependence of the Correlation between Ozone and Temperature Oscillations in the Middle Atmosphere. Atmosphere 2023, 14, 1436.
Abstract
This study investigates the frequency dependence of the correlation or anticorrelation of ozone and temperature in the middle atmosphere. The anticorrelation of ozone and temperature plays a role for the expected recovery or superrecovery of upper stratospheric ozone in presence of manmade cooling of the middle atmosphere due to increasing carbon dioxide emissions. The correlation between lower stratospheric ozone and temperature indicates the dependence of lower stratospheric temperature trends on the ozone evolution in addition to greenhouse gas emissions. Ozone and temperature measurements of the microwave limb sounder (MLS) on the satellite Aura from 2004 to 2021 are utilized for Bern (46.95∘N, 7.44∘E) at middle latitudes and for the equator region. The time series are bandpass filtered for periods from 2 days to 5 years. The correlation coefficient depends on the period of the oscillation in temperature and ozone. The strongest correlation and anticorrelation are found for the annual oscillation. The anticorrelation between ozone and temperature in the upper stratosphere is about −0.7 at a period of 2 days and −0.99 at a period of one year. Thus, the temperature dependence of the ozone reaction rates also leads to an anticorrelation of ozone and temperature at short periods so that ozone can be considered as a tracer of planetary waves. At the equator, a dominant semiannual oscillation and an 11 year solar cycle are found for nighttime ozone in the upper mesosphere. The SAO in ozone and temperature show a strong correlation indicating a dynamical control of the ozone SAO in the upper mesosphere. The SAO in the equatorial nighttime values of ozone and temperature is due to a semiannual modulation of vertical advection by the diurnal tide.
Environmental and Earth Sciences, Atmospheric Science and Meteorology
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