Gas fluxes and steady state saturation anomalies at very high wind speeds

dc.contributor.author Stanley, Rachel H. R.
dc.contributor.author Kinjo, Lumi
dc.contributor.author Smith, Andrew W.
dc.contributor.author Aldrett, Danielle
dc.contributor.author Alt, Helene
dc.contributor.author Kopp, Emily
dc.contributor.author Krevanko, Callan
dc.contributor.author Cahill, Kevin
dc.contributor.author Haus, Brian K.
dc.date.accessioned 2023-04-20T20:03:57Z
dc.date.available 2023-04-20T20:03:57Z
dc.date.issued 2022-09-25
dc.description Author Posting. © American Geophysical Union, 2022. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Journal of Geophysical Research: Oceans 127(10), (2022): e2021JC018387, https://doi.org/10.1029/2021jc018387.
dc.description.abstract Gas exchange at high wind speeds is not well understood—few studies have been conducted at wind speeds above 20 ms−1 and significant disagreement exists between gas exchange models at high wind speeds. In this study, noble gases (He, Ne, Ar, Kr, and Xe) were measured in 35 experiments in the SUSTAIN wind‐wave tank where the wind speeds ranged from 20 to 50 m s−1 and mechanical waves were generated as monochromatic or with a short‐crested JONSWAP frequency spectrum. Bubble size spectra were determined using shadowgraph imagery and wave statistics were measured using a wave wire array. The steady state saturation anomalies and gas fluxes initially increased as wind speeds increased but then leveled off, similar to prior studies of heat and momentum flux coefficients. Noble gas fluxes and steady state saturation anomalies are correlated most strongly with bubble volumes for the less soluble noble gases and with wind speed and wave Reynolds number for the more soluble noble gases. In the JONSWAP experiments, significant wave height was the most important predictor for gas steady state saturation anomalies with correlation coefficients of greater than 0.92 for He, Ne, and Ar (P < 0.05). Furthermore, invasion fluxes were larger than evasion fluxes when other conditions were similar. Taken together, these lab‐based experiments suggest more attention should be paid to parameterizations based on wave characteristics and bubbles and that current wind‐speed based gas exchange parameterizations should not be applied to conditions with very high wind speeds.
dc.description.sponsorship This work was supported by the National Science Foundation (Grant OCE1634467 and OCE1634432). We are grateful for the assistance of members of the SUSTAIN lab at the University of Miami for assistance in setting up the experiments and collecting data and to William Jenkins and Dempsey Lott of the WHOI Isotope Geochemistry Facility for noble gas analysis of copper tube samples. We also are grateful for the GitHub gas toolbox of David Nicholson and Cara Man (https://github.com/dnicholson/gas_toolbox) that was used to calculate gas fluxes from the S09, L13, and N16 parameterizations
dc.identifier.citation Stanley, R., Kinjo, L., Smith, A., Aldrett, D., Alt, H., Kopp, E., Krevanko, C., Cahill, K., & Haus, B. (2022). Gas fluxes and steady state saturation anomalies at very high wind speeds. Journal of Geophysical Research: Oceans, 127(10), e2021JC018387.
dc.identifier.doi 10.1029/2021jc018387
dc.identifier.uri https://hdl.handle.net/1912/66007
dc.publisher American Geophysical Union
dc.relation.uri https://doi.org/10.1029/2021jc018387
dc.subject Air-sea gas exchange
dc.subject Bubbles
dc.subject Noble gases
dc.subject High winds
dc.subject Saturation anomaly
dc.subject SUSTAIN
dc.title Gas fluxes and steady state saturation anomalies at very high wind speeds
dc.type Article
dspace.entity.type Publication
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relation.isAuthorOfPublication.latestForDiscovery 7383eed8-6eca-47d1-a1cc-452ea1e35eca
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