Wet chemical surface ozone measurements during POLARSTERN cruise ANT-IV/1a, ANT-IV/1b, ANT-IV/1c, ANT-IV/2 and ANT-IV/3 (PS08) in 1985

DOI

The destinations are described in Fütterer (1986). The high ozone peak at 20°N could have been caused by an intrusion of stratospheric ozone at the subtropical tropopause break. The ITCZ on the outward journey at 3°N was localized at the wind jump.

Please note: if only latitude is given then this information is approximate.

Identifier
DOI https://doi.org/10.1594/PANGAEA.949146
Related Identifier References https://doi.org/10.2312/BzP_0032_1986
Related Identifier References 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.949146
Provenance
Creator Winkler, Peter
Publisher PANGAEA
Publication Year 2022
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 2242 data points
Discipline Earth System Research
Spatial Coverage (-70.783W, -73.973S, -8.195E, 48.600N); North Sea
Temporal Coverage Begin 1985-09-05T09:00:00Z
Temporal Coverage End 1985-12-22T21:00:00Z