Articles | Volume 20, issue 6
https://doi.org/10.5194/os-20-1441-2024
https://doi.org/10.5194/os-20-1441-2024
Research article
 | 
05 Nov 2024
Research article |  | 05 Nov 2024

Upper-ocean changes with hurricane-strength wind events: a study using Argo profiles and an ocean reanalysis

Jacopo Sala, Donata Giglio, Addison Hu, Mikael Kuusela, Kimberly M. Wood, and Ann B. Lee

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Cited articles

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Argo: Argo float data and metadata from global data assembly centre (Argo GDAC), Seanoe [data set], https://doi.org/10.17882/42182, 2000. a, b, c
Balaguru, K., Chang, P., Saravanan, R., Leung, L. R., Xu, Z., Li, M., and Hsieh, J.-S.: Ocean barrier layers' effect on tropical cyclone intensification, P. Natl. Acad. Sci. USA, 109, 14343–14347, 2012. a, b, c, d, e
Balaguru, K., Foltz, G. R., Leung, L. R., and Emanuel, K. A.: Global warming-induced upper-ocean freshening and the intensification of super typhoons, Nat. Commun., 7, 1–8, 2016. a
Balaguru, K., Foltz, G. R., and Leung, L. R.: Increasing magnitude of hurricane rapid intensification in the central and eastern tropical Atlantic, Geophys. Res. Lett., 45, 4238–4247, 2018. a
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Short summary
As Earth’s climate warms, cyclone intensity and rain may increase. Cyclones, like hurricanes, gain strength from warm ocean waters. Understanding how oceans react to strong winds is vital. We highlight ocean responses to pre-storm salinity. Changes in salinity affect oceans during storms: salinity rises, temperature falls, and density increases. We suggest that mixing of near-surface with deeper water may impact heat exchange between the ocean and atmosphere during and after a weather event.
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