Abstract
Daily Total Column Ozone (TCO) measurements compiled from Total Ozone Mapping Spectrometer (TOMS) and Ozone Monitoring Instruments (OMI) were used to analyze the global and hemispherical TCO interannual variations. Two periods of TCO measurements were analyzed separately covering full years. For the 1978-1994 period, the TCO showed a global decade decrease rate of 13.45 DU (about -4.3%). For the Northern Hemisphere(NH) the decade decrease rate was of 12.96 DU (-4.0%), while in the Southern Hemisphere (SH) was of 13.57 DU (-4.5%). These decreases in ozone trends, using the totality of TOMS and OMI satellite measurements, are greater than those reported in literature. The 1998-2014 period global TCO decade decrease rate was of 1.56 DU, corresponding 0.94 DU and 0.138 DU for the NH and SH, respectively. The global TCO variations must show a double annual periodicity, the first one with maxima in March due to the Northern Hemisphere (NH) and the second one during September due to the Southern Hemisphere (SH). However, the maxima due to SH TCO interannual variations have gradually vanished. A disturbance in the SH TCO interannual variations has appeared since 1980; graphically the periodicity brakes down and transforms to a double peak from 1985 and on. This effect can be attributed to the hemispheric impact of the ozone hole at the South Pole. Between October 1, 2004 and December 14, 2005 TOMS and OMI have recorded this disturbance unequivocally. We conclude that the disturbance in SH TCO has an irreversible character.
Highlights
Atmospheric Ozone is formed by photo-dissociation induced by UV-C solar radiation in oxygen molecules
Total Column Ozone (TCO) measurements compiled from Total Ozone Mapping Spectrometer (TOMS) and Ozone Monitoring Instruments (OMI) were used to analyze the global and hemispherical TCO interannual variations
For the Northern Hemisphere(NH) the decade decrease rate was of 12.96 Dobson Units (DU) (−4.0%), while in the Southern Hemisphere (SH) was of 13.57 DU (−4.5%)
Summary
Atmospheric Ozone is formed by photo-dissociation induced by UV-C solar radiation in oxygen molecules. Non-simulation has been used, and TCO direct values were used from TOMS and OMI data It is assumed, that to know their behavior is necessary to assess the total ozone amount in the whole atmosphere. The polar nights affect the daily global coverage; it does not manage to cover a significant region, which reaches a maximum 29 ̊ of latitude near the poles on solstices: June 21st-22nd, for the SH and December 21st-22nd, for the Northern Hemisphere. TCO analysis was performed from daily files of measurements covering more than 75% of earth observation parcels; the total number of observable parcels was 51,840 and 64,800 for TOMS and OMI, respectively.
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