New System to Measure Carbonyl Sulfide in Air Samples from Baring Head and Fiordland National Park, New Zealand
P. Sperlich1, G. Brailsford1, K.T. Puni2, J. McGregor1, R. Moss1, S. Nichol1, S. Mikaloff-Fletcher1, B. Bukosa1, B. Hall3 and S. Montzka3
1National Institute of Water and Atmospheric Research (NIWA), Wellington, New Zealand; 043860855, E-mail: firstname.lastname@example.org
2National Institute of Water and Atmospheric Research, Wellington, New Zealand
3NOAA Global Monitoring Laboratory (GML), Boulder, CO 80305
One of the largest uncertainties in future climate predictions stems from the uncertainty of future atmospheric CO2 levels. In order to make robust predictions of the atmospheric CO2 load, a sound understanding of present-day CO2 fluxes is vital. Measurements of carbonyl sulfide (COS) have been suggested as a powerful tracer for gross primary production (GPP) as the most significant flux of terrestrial CO2 uptake.
We are currently developing a new analytical system that combines a commercial, continuous-flow COS analyser (Los Gatos Research) with a custom-build sample inlet for measurements of COS in flask samples (Fig. 1). We describe the instrument components as well as our strategy for quality control and instrument calibration. This allows an assessment of the measurement performance we currently achieve. Finally, we will show first results from Baring Head (BHD), our Southern Hemisphere baseline observatory and measurements of air samples taken in Fiordland National Park, a native forest at the south-western tip of New Zealand’s South Island.
The presented system will support CarbonWatch NZ, a research programme to quantify national CO2 fluxes in New Zealand.
Figure 1. Figure 1: Schematic of the measurement system for COS at NIWA.