Two decades of flask observations of atmospheric δO2/N2, CO2, and APO at stations Lutjewad (the Netherlands) and Mace Head (Ireland) plus 3 years from Halley station (Antarctica)

DOI

This is the data supplement presented in Nguyen et al. 2021 (https://doi.org/10.5194/essd-2021-213) in which we present 20-year flask sample records of atmospheric CO2, δO2/N2 and APO from the stations Lutjewad (the Netherlands) and Mace Head (Ireland) and a 3-year record from Halley station (Antarctica), including details of the extensive calibration procedure and its stability over time. The results of our inter-comparison involving gas cylinders from various research laboratories worldwide also show that our calibration is of high quality and compatible with the internationally-recognised Scripps scale. The measurement records from Lutjewad and Mace Head show similar long-term trends during the period 2002-2018 of 2.31 ± 0.07 ppm yr-1 for CO2 and -21.2 ± 0.8 per meg yr-1 for δO2/N2 at Lutjewad, and 2.22 ± 0.04 ppm yr-1 for CO2 and -21.3 ± 0.9 per meg yr-1 for δO2/N2 at Mace Head. They also show similar δO2/N2 seasonal cycle with an amplitude of 54 ± 4 per meg at Lutjewad and 61 ± 5 per meg at Mace Head, while CO2 seasonal amplitude at Lutjewad (16.8 ± 0.5 ppm) is slightly higher than that at Mace Head (14.8 ± 0.3 ppm). We show that the observed trends and seasonal cycles are compatible with the measurements from various stations, especially the measurements from Weybourne Atmospheric Observatory (United Kingdom). However, there are remarkable differences in the progression of annual trends between the Mace Head and Lutjewad records for δO2/N2 and APO, which might in part be caused by sampling differences, but also by environmental effects, such as the North Atlantic Ocean oxygen ventilation changes to which Mace Head is more sensitive. The Halley record shows clear trends and seasonality in δO2/N2 and APO, where especially APO agrees well with the continuous measurements at Halley by the University of East Anglia, while CO2 and δO2/N2 present slight disagreements, most likely caused by small leakages during sampling. From our 2002-2018 records, we find good agreement for the global ocean sink: 2.0 ± 0.8 PgC yr-1 and 2.2 ± 0.9 PgC yr-1, based on Lutjewad and Mace Head, respectively.

Identifier
DOI https://doi.org/10.18160/QQ7D-T060
Related Identifier https://doi.org/10.5194/essd-13-2307-2021
Metadata Access https://oai.datacite.org/oai?verb=GetRecord&metadataPrefix=datacite&identifier=doi:10.18160/qq7d-t060
Provenance
Creator Nguyen, Linh N.T. ORCID logo; Luijkx, Ingrid ORCID logo; Meijer, Harro A.J. ORCID logo
Publisher ICOS ERIC - Carbon Portal
Publication Year 2021
Funding Reference Nederlandse Organisatie voor Wetenschappelijk Onderzoek ; FP7 Environment 511176 Carbo-Ocean
Rights Creative Commons Attribution 4.0 International; https://creativecommons.org/licenses/by/4.0/legalcode
OpenAccess true
Representation
Resource Type ZIP archive; Collection
Format Collection of CSV files in a zip archive
Size 115 KB
Version 2.0
Discipline Other
Spatial Coverage (53.404 LON, 6.353 LAT); Lutjewad; Mace Head; Halley