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Correction: Dynamics of Upwelling and Downwelling in a Channel Basin of the Baltic Sea Cover

Correction: Dynamics of Upwelling and Downwelling in a Channel Basin of the Baltic Sea

Open Access
|May 2026

Figures & Tables

Corrected Caption Figure 7

Instability diagnostics after the onset of instability (ti = 6) for UPSLOPE, summer. (a): Thermal wind overlapped with contours of cpe (purple lines) and cmke (green lines). Contour lines show the interval (0.4, 1.6) · 10–8, with every interval given by 0.4 · 10–8. Thermocline and halocline are given by the dashed red and green lines, respectively. The vertical solid black line marks the frontal jet location alongshore section in (c) is taken. (b) PV field superimposed on the contours of alongshore velocity (coastal jet; black lines). (c) Alongshore section of normalized cross-shore velocity uw at the frontal jet location (black solid line in (a)).

Figure 8

Same as Figure 7 but for DOWNSLOPE, summer, ti = 18.

Corrected Caption Figure 4

A schematic summary of the instability diagnostics for the different model configurations. EKE is given in 10–6 m2 s–2. Growth rate in day–1. See text for details. Signs in the brackets in the bottom two rows (PV gradient condition) refer to the sign of the cross-shore PV gradient.

Language: English
Page range: 68 - 72
Submitted on: May 5, 2026
Accepted on: May 5, 2026
Published on: May 18, 2026
Published by: Stockholm University Press
In partnership with: Paradigm Publishing Services

© 2026 Matteo Masini, Inga Monika Koszalka, Johan Nilsson, Alexander Sokolov, Bo Gustafsson, published by Stockholm University Press
This work is licensed under the Creative Commons Attribution 4.0 License.