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.

Bibliographic Details
Main Author:	Winkler, Peter
Format:	Dataset
Language:	English
Published:	PANGAEA 2022
Subjects:	ANT-IV/1a ANT-IV/1b ANT-IV/1c ANT-IV/2 ANT-IV/3 CT DATE/TIME Electrochemical concentration cell (ECC) (Atmannspacher 1971) Event label LATITUDE LONGITUDE Ozone Polarstern PS08 PS08/1a-track PS08/1b-track PS08/1c-track PS08/2-track PS08/3-track PS08 NOAMP Underway cruise track measurements Berichte zur Polar- und Meeresforschung Berichte zur Polarforschung Polar Research Polarforschung Reports on Polar and Marine Research Reports on polar research
Online Access:	https://doi.pangaea.de/10.1594/PANGAEA.949146 https://doi.org/10.1594/PANGAEA.949146

Description
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.