Ryo Dobashi, David T. Ho, Yuanxu Dong, Christa A. Marandino, and Helen Czerski
Air-sea CO2 fluxes play an important role in the global carbon cycle and impact Earth's climate. Knowledge of the gas transfer velocity (k) is needed to determine air-sea CO2 fluxes, and wind speed-based parametrizations of k often perform well in the open ocean under moderate winds. In the Baltic Sea, several parameterizations have been proposed to estimate k, and they yield a higher k compared with parameterizations commonly used in the open ocean. In this study, we measured k in the Baltic Sea using the 3He/SF6 dual tracer technique to assess the applicability of published parameterizations in the inland sea ecosystem. Observed k was similar to those in offshore regions at the same wind speeds, even with enhanced surfactant activity. Comparison with observations in the nearshore Baltic Sea suggests that commonly used open ocean parameterizations are applicable in the Baltic Sea under moderate wind speeds and developed wave fields.
Received: 14 Apr 2026 – Discussion started: 22 Apr 2026
Publisher's note: Copernicus Publications remains neutral with regard to jurisdictional claims made in the text, published maps, institutional affiliations, or any other geographical representation in this paper. While Copernicus Publications makes every effort to include appropriate place names, the final responsibility lies with the authors. Views expressed in the text are those of the authors and do not necessarily reflect the views of the publisher.
Ryo Dobashi, David T. Ho, Yuanxu Dong, Christa A. Marandino, and Helen Czerski
Data sets
Dataset: Sulfur hexafluoride and helium data from a tracer release experiment conducted in July 2022 in the central Baltic Sea during research cruise EMB295 on the R/V Elisabeth Mann Borgese
David T. Ho and Ryo Dobashi
https://www.bco-dmo.org/dataset/988658
Ryo Dobashi, David T. Ho, Yuanxu Dong, Christa A. Marandino, and Helen Czerski
Metrics will be available soon.
Latest update: 22 Apr 2026