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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Format: | Dataset |
Language: | English |
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PANGAEA
2024
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Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.966584 https://doi.org/10.1594/PANGAEA.966584 |