Dispersion of deep-sea hydrothermal plumes at the Endeavour Segment of the Juan de Fuca Ridge: a multiscale numerical study
- 1Applied Physics Laboratory, University of Washington, Seattle, WA, United States
- 2Geology & Geophysics, Woods Hole Oceanographic Institution, Woods Hole, MA, United States
A Corrigendum on
Dispersion of deep-sea hydrothermal plumes at the Endeavour Segment of the Juan de Fuca Ridge: a multiscale numerical study
By Xu G and German CR (2023). Front. Mar. Sci. 10:1213470. doi: 10.3389/fmars.2023.1213470
In the published article, there was an error. The formulas in Equations 1 and 2 and the inline formula in the text that follows are incorrect. We apologize for not catching this typesetting error during the proof review. A correction has been made to these formulas in Section 4.1 Flow velocity time series.
The original formulas in Equations 1 and 2 are:
and
The corrected formulas appear below:
and
In the text below these two equations, on the third line, the inline formula in the published article is “(e.g., ).”
The corrected formula appears below:
The authors apologize for this error and state that this does not change the scientific conclusions of the article in any way. The original article has been updated.
Publisher’s note
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Keywords: numerical model, hydrothermal vent, plume dispersion, tidal forcing, buoyancy, mixing
Citation: Xu G and German CR (2024) Corrigendum: Dispersion of deep-sea hydrothermal plumes at the Endeavour Segment of the Juan de Fuca Ridge: a multiscale numerical study. Front. Mar. Sci. 11:1532941. doi: 10.3389/fmars.2024.1532941
Received: 22 November 2024; Accepted: 26 November 2024;
Published: 09 December 2024.
Edited and Reviewed by:
Shi-Di Huang, Southern University of Science and Technology, ChinaCopyright © 2024 Xu and German. This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) and the copyright owner(s) are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.
*Correspondence: Guangyu Xu, Z3Vhbmd5dXhAdXcuZWR1