Abstract
Extensive observations of total column ozone (TCO) made over the Antarctic region at the Indian station ‘Maitri’ (70.76oS, 11.74oE) during two summer periods of 2004–2005 and 2006–2007 using a ground-based optical remote sensing instrument (ozonometer) have been examined to study the short-term variations. Mean TCO during 2004–05 summer was 288.7 DU with a variability of 8% and the corresponding values during 2006–2007 summer were 280.4 DU and 11%. Both ozonometer and Dobson spectrophotometer measurements at this Antarctic station during January 2005 showed a short-term decrease in TCO by about 70 DU before regaining original value. Simultaneous changes in precipitable water and surface temperature points to a possible interplay of chemistry and meteorological conditions. Occurrence of an intense solar proton event in January 2005 also suggests the possible role of precipitating charged particles in causing short-lived ozone decrease through production of OH radical.
Acknowledgements
The authors are grateful to the Director of the Indian Institute of Tropical Meteorology, Pune for support and encouragement. Support received from the scientists of National Center for Antartic and Ocean Research (NCAOR), Goa and from the Department of Ocean Development/Ministry of Earth Sciences, Government of India by facilitating participation of one of the authors (SMS) in two Indian summer expeditions to Antarctica is gratefully acknowledged.