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

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 requir...

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Bibliographic Details
Main Author: Winkler, Peter
Format: Dataset
Language:English
Published: PANGAEA 2024
Subjects:
ANT-VI/1
ANT-VI/2
CT
DATE/TIME
Electrochemical concentration cell (ECC) (Atmannspacher 1971)
Event label
LATITUDE
LONGITUDE
Ozone
Polarstern
PS12
PS12/1-track
PS12/2-track
Underway cruise track measurements
Berichte zur Polar- und Meeresforschung
Reports on Polar and Marine Research
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.966584
https://doi.org/10.1594/PANGAEA.966584
Description
Summary: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.

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