Daily readings of total column ozone over Macquarie Island
This dataset was originally set up as a "State of the Environment" indicator - however, that application no longer functions at the Australian Antarctic Data Centre, so the data have been extracted and attached to this original metadata record for the indicator. These data are a locally he...
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| Format: | Dataset |
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Australian Antarctic Data Centre
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| Online Access: | https://researchdata.edu.au/daily-readings-total-macquarie-island/701758 https://data.aad.gov.au/metadata/records/SOE_ozone http://nla.gov.au/nla.party-617536 |
| Summary: | This dataset was originally set up as a "State of the Environment" indicator - however, that application no longer functions at the Australian Antarctic Data Centre, so the data have been extracted and attached to this original metadata record for the indicator. These data are a locally held AADC copy of data from the WOUDC (updated annually). INDICATOR DEFINITION The monthly means of total column ozone measured at Macquarie Island. RATIONALE FOR INDICATOR SELECTION Ozone filters ultra-violet (UV) radiation from the Sun and affects the dynamics of the stratosphere and overall atmospheric radiation balance. With reduction in stratospheric ozone levels, UV incidence on the surface has serious ramifications for Antarctic and Southern Ocean biological systems. DESIGN AND STRATEGY FOR INDICATOR MONITORING PROGRAM Spatial Scale: Macquarie Island (lat 54 deg 29' 59"S, long 158 deg 57' 08"E). Measurement Technique: Global-scale daily analyses are produced by the Bureau of Meteorology on a 2.5 - degree latitude by 2.5 - degree longitude grid, using satellite data. In-situ Dobson spectrophotometer measurements at Macquarie Island in conjunction with major centres in Australia provide benchmark and calibration data of total-column ozone. Macquarie Island is the only station situated under the Antarctic Ozone hole, providing an important contribution to ozone monitoring activities. RESEARCH ISSUES The traceable data set may be extended back a few years before 1978 but cannot go much further back with any confidence. When Dobson measurements began seriously in 1955, there was no traceability of instrument standards. Each instrument was calibrated absolutely rather than by the hierarchy of standards, beginning in 1978. In the initial measurement program, ozone measurements were used mainly for day-to-day variations - the idea of using Dobsons for a long-term trend in ozone was not an objective. Consequently the need for properly referenced instruments was not a high priority. The difficult mechanism of applying standards was not in place when measurements started in 1956. Data collection is ongoing. |
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