ID:
publications-1438
Type:
PEER REVIEWED ARTICLE
Year:
2015
Authors:
Anita VÔrai , Viktória Homonnai , Imre M. JÔnosi , Rolf Müller
Title:
Early signatures of ozone trend reversal over the Antarctic
Venue/Journal:
DOI:
10.1002/2014ef000270
Research type:
Data Management & Analytics
Water System:
Precipitation & Ecological Systems
Technical Focus:
Abstract:
AbstractWe report on a detailed time series analysis of long total column ozone (TO) records based on multiāsatellite observations of daily resolution. We concentrate on three geographic latitudes over and around the Antarctic area, specifically on three circles at 58.5°S, 59.5°S, and 79.5°S. Almost continuous observations are available at the two former latitudes; however, data are lacking during the polar winter periods at 79.5°S, because the measurement technique requires sunlight. The methodology is motivated by levelācrossing statistics, where subsets of the records above or below particular threshold levels are evaluated. Longāterm trend reversal at around the turn of the century is already detectable for low TO levels in the raw time series in the āozoneāholeā region (79.5°S). In order to overcome the apparent nonāstationarities of the time series, we determined daily TO differences (ĪTO) belonging to the same geographic longitudes between the different latitudinal circles. The result is a stable, stationary behavior for small (absolute) ĪTO values in the period JanuaryāFebruaryāMarch without any significant detectable trends. The high absolute value ĪTO subsets (SeptemberāOctoberāNovember) indicate a robust trend reversal in the middle of the 1990s. The observed trend reversal in the total column ozone time series is consistent with the temporal development of the stratospheric halogen loading. However, a close correspondence of ozone and halogen turnaround years is not expected because of the statistical uncertainties in the determination of the ozone turnaround, and the many factors contributing to ozone depletion processes.
Link with Projects:
603557
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