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
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.
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Format: | Dataset |
Language: | English |
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PANGAEA
2022
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Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.949146 https://doi.org/10.1594/PANGAEA.949146 |
Summary: | 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. |
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