The CSIRO-BoM-AAD Antarctic and Southern Ocean atmospheric monitoring network
The CSIRO-BoM-AAD Antarctic and Southern Ocean atmospheric monitoring network
Authors
Marcel van der Schoot, Ann Stavert and David Etheridge
Centre for Australian Weather and Climate Research, CSIRO Marine and Atmospheric Research Aspendale, Victoria, Australia
Abstract
Gases released by human activity (greenhouse and ozone depleting gases) are responsible for global change. They are long-lived and well-mixed in the atmosphere. The Antarctic regions, remote from industrial and land plant activity are ideally located to measure global changes in the gases. The CSIRO sampling network, in conjunction with the Bureau of Meteorology and the Australian Antarctic Division, represents the most comprehensive, long-running Southern Hemisphere program. With continuing innovation in measurement and interpretive models, it has been used to detect regional changes in carbon uptake, and together with other measurement sites monitor global changes in emissions and uptake of several gases.
Measurements of CO2, methane (CH4), carbon monoxide (CO), hydrogen (H2), nitrous oxide (N2O), and the stable isotopes of CO2 have been made in fortnightly flask air samples since the early 1990s, at CSIRO. Measurements of carbon 14 in CO2, oxygen concentrations, and radon concentrations have been made by our collaborators. The measurements have been used to detect variations and trends in the gases, and relate them to natural and anthropogenic emissions and natural sinks. Recent developments include the installation of a new breed of continuous in situ analysers for a growing number of these species, which provides improved frequency and precision of measurements as well as several operational advantages.
These data continue to be used, along with measurements from other baseline sites across the globe, in inverse studies that derive regional sources and sinks and their trends. From this, the processes behind variations in gas emissions and uptake can be better understood so that future model predictions of greenhouse gas levels and their climate impact can be improved.

