Wet chemical surface ozone measurements during POLARSTERN cruise ANT-VI/1-2 (PS12) in 1987

DOI

The destinations are described in Fütterer (1986). It is possible that the high ozone peak at 22.5°S may be due to both stratospheric intrusion and long-distance transport from areas of biomass burning. The maximum biomass combustion occurs in September to November. A more complex analysis is required to clarify the contributions from both sources.

Please note, that the positions were taken from the Mastertracks, sometimes no positions available for certain periods.

Identifier
DOI https://doi.org/10.1594/PANGAEA.966584
Related Identifier https://doi.org/10.48433/BzPM_0760_2022
Metadata Access https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.966584
Provenance
Creator Winkler, Peter
Publisher PANGAEA
Publication Year 2024
Rights Creative Commons Attribution 4.0 International; https://creativecommons.org/licenses/by/4.0/
OpenAccess true
Representation
Resource Type Dataset
Format text/tab-separated-values
Size 568 data points
Discipline Earth System Research
Spatial Coverage (-57.036W, -63.389S, -18.369E, 29.164N)
Temporal Coverage Begin 1987-10-04T12:00:00Z
Temporal Coverage End 1987-10-30T18:00:00Z