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Global and Hemispherical Interannual Variation of Total Column Ozone from TOMS and OMI Data

Global and Hemispherical Interannual Variation of Total Column Ozone from TOMS and OMI Data

作     者:José Luis Pinedo-Vega Mario Molina-Almaraz Carlos Ríos-Martínez Fernando Mireles-García J. Ignacio Dávila-Rangel 

作者机构:Universidad Autónoma de Zacatecas (UAEN) Ciprés 10 Fracc. La Peñuela Zacatecas México 

出 版 物:《Atmospheric and Climate Sciences》 (大气和气候科学(英文))

年 卷 期:2017年第7卷第3期

页      面:247-255页

学科分类:07[理学] 0706[理学-大气科学] 

主  题:Global and Hemispherical Ozone Trends Total Column Ozone Interannual Variation TOMS Data OMI Data 

摘      要: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.

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