Upper ocean response to Hurricane Gonzalo 2014: salinity effects revealed by targeted and sustained underwater glider observations.
Open accessAbstract
During October 2014, Hurricane Gonzalo traveled within 85 km from the location of an underwater glider situated north of Puerto Rico. Observations collected before, during, and after the passage of this hurricane were analyzed to improve our understanding of the upper ocean response to hurricane winds. The main finding in this study is that salinity potentially played an important role on changes observed in the upper ocean; a near‐surface barrier layer likely suppressed the hurricane‐induced upper ocean cooling, leading to smaller than expected temperature changes. Poststorm observations also revealed a partial recovery of the ocean to prestorm conditions 11 days after the hurricane. Comparison with a coupled ocean‐atmosphere hurricane model indicates that model‐observations discrepancies are largely linked to salinity effects described. Results presented in this study emphasize the value of underwater glider observations for improving our knowledge of how the ocean responds to tropical cyclone winds and for tropical cyclone intensification studies and forecasts.
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In the northwestern tropical Atlantic, the Amazon-Orinoco plume increases salinity stratification, limiting hurricane-induced SST cooling.
“This is especially true in the northwestern tropical Atlantic, where the Amazon-Orinoco plume increases salinity stratification, limiting hurricane-induced SST cooling (Figure 5; Balaguru et al., 2012;Grodsky et al., 2012b;Domingues et al., 2015).”
From The tropical atlantic observing system (2019) · cites this paper as Domingues et al., 2015
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- Abarbanel, H. D., D. D. Holm, J. E. Marsden, and T. Ratiu (1984), Richardson number criterion for the nonlinear stability of three-dimensional stratified flow, Phys. Rev. Lett., 52(26), 2352.
- Balaguru, K., P. Chang, R. Saravanan, L. R. Leung, Z. Xu, M. Li, and J. S. Hsieh (2012b), Ocean barrier layers' effect on tropical cyclone intensification, Proc. Natl. Acad. Sci. U.S.A., 109(36), 14,343-14,347.
- Brink, K. H. (1989), Observations of the response of thermocline currents to a hurricane, J. Phys. Oceanogr., 19(7), 1017-1022.
- Corredor, J., J. Morell, J. López, R. Armstrong, A. Dieppa, C. Cabanillas, A. Cabrera, and V. Hensley (2003), Remote continental forcing of phytoplankton biogeochemistry: Observations across the "Caribbean-Atlantic front", Geophys. Res. Lett., 30(20), 2057, doi:10.1029/ 2003GL018193. · DOI
- Dickey, T., D. Frye, J. McNeil, D. Manov, N. Nelson, D. Sigurdson, H. Jannasch, D. Siegel, T. Michaels, and R. Johnson (1998), Upper-ocean temperature response to Hurricane Felix as measured by the Bermuda testbed mooring, Mon. Weather Rev., 126(5), 1195-1201.
- Goni, G., J. A. Knaff, and I.-I. Lin (2015), State of the climate in 2014, Bull. Am. Meteorol. Soc., 96(7), S121-S122.
- Grodsky, S. A., N. Reul, G. Lagerloef, G. Reverdin, J. A. Carton, B. Chapron, Y. Quilfen, V. N. Kudryavtsev, and H.-Y. Kao (2012), Haline hurricane wake in the Amazon/Orinoco plume: AQUARIUS/SACD and SMOS observations, Geophys. Res. Lett., 39, L20603, doi:10.1029/2012GL053335. · DOI
- Johns, E. M., B. A. Muhling, R. C. Perez, F. E. Müller-Karger, N. Melo, R. H. Smith, J. T. Lamkin, T. L. Gerard, and E. Malca (2014), Amazon River water in the northeastern Caribbean Sea and its effect on larval reef fish assemblages during April 2009, Fish. Oceanogr., 23(6), 472-494.
- Kelly, P. S., K. M. Lwiza, R. K. Cowen, and G. J. Goni (2000), Low-salinity pools at Barbados, West Indies: Their origin, frequency, and variability, J. Geophys. Res., 105(C8), 19,699-19,708, doi:10.1029/1999JC900328. · DOI
- Landsea, C. W. (1993), A climatology of intense (or major) Atlantic hurricanes, Mon. Weather Rev., 121(6), 1703-1713.
- Lin, I. I., C. C. Wu, I. F. Pun, and D. S. Ko (2008), Upper-ocean thermal structure and the western North Pacific Category 5 typhoons. Part I: Ocean features and the Category 5 typhoons' intensification, Mon. Weather Rev., 136(9), 3288-3306.
- Lin, I. I., G. J. Goni, J. A. Knaff, C. Forbes, and M. M. Ali (2013), Ocean heat content for tropical cyclone intensity forecasting and its impact on storm surge, Nat. Hazards, 66(3), 1481-1500.
- Locarnini, R. A., et al. (2013), World Ocean Atlas 2013, Temp., NOAA Atlas NESDIS 73, vol. 1, edited by S. Levitus and A. Mishonov, 40 pp., NOAA, Silver Spring, Md.
- Mainelli, M., M. DeMaria, L. Shay, and G. Goni (2008), Application of oceanic heat content estimation to operational forecasting of recent Atlantic Category 5 hurricanes, Weather Forecasting, 23(1), 3-16.
- Miles, J. W. (1961), On the stability of heterogeneous shear flows, J. Fluid Mech., 10(04), 496-508.
- Prasad, T. G., and P. J. Hogan (2007), Upper-ocean response to Hurricane Ivan in a 1/25 nested Gulf of Mexico HYCOM, J. Geophys. Res., 112, C04013, doi:10.1029/2006JC003695. · DOI
- Price, J. F. (1981), Upper-ocean response to a hurricane, J. Phys. Oceanogr., 11(2), 153-175.
- Price, J. F., T. B. Sanford, and G. Z. Forristall (1994), Forced stage response to a moving hurricane, J. Phys. Oceanogr., 24(2), 233-260.
- Sanford, T. B., P. G. Black, J. R. Haustein, J. W. Feeney, G. Z. Forristall, and J. F. Price (1987), Ocean response to a hurricane. Part I: Observations, J. Phys. Oceanogr., 17(11), 2065-2083.
- Shay, L. K., G. J. Goni, and P. G. Black (2000), Effects of a warm oceanic feature on Hurricane Opal, Mon. Weather Rev., 128(5), 1366-1383.
- Sprintall, J., and M. Tomczak (1992), Evidence of the barrier layer in the surface layer of the tropics, J. Geophys. Res., 97(C5), 7305-7316, doi:10.1029/92JC00407. · DOI
- Vissa, N. K., A. N. V. Satyanarayana, and B. P. Kumar (2013), Response of upper ocean and impact of barrier layer on Sidr cyclone induced sea surface cooling, Ocean Sci. J., 48(3), 279-288.
- Walker, N. D., R. R. Leben, and S. Balasubramanian (2005), Hurricane-forced upwelling and chlorophyll a enhancement within cold-core cyclones in the Gulf of Mexico, Geophys. Res. Lett., 32, L18610, doi:10.1029/2005GL023716. · DOI
- Zweng, M. M., et al. (2013), World Ocean Atlas 2013, Salinity, NOAA Atlas NESDIS 74, vol. 2, edited by S. Levitus and A. Mishonov, 39 pp., NOAA, Silver Spring, Md. Geophysical Research Letters 10.1002/2015GL065378
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Foltz, G. R., Brandt, P., Richter, I., Rodríguez-Fonseca, B., Hernandez, F., Dengler, M., Rodrigues, R. R., Schmidt, J. O., Yu, L., Lefevre, N., et al. (2019) · Frontiers in Marine Science · doi:10.3389/fmars.2019.00206 · Cited by 150 · see citing works
- Authors
- Domingues, R., Goni, G., Bringas, F., Lee, S., Kim, H., Halliwell, G., Dong, J., Morell, J., & Pomales, L.
- Affiliations
- National Oceanic and Atmospheric Administration (US)
- Caribbean Coastal Ocean Observing System (PR)
- University of Puerto Rico Mayaguez Mayaguez Puerto Rico
- Corresponding author
- Domingues, Ricardo
- Venue
- Geophysical Research Letters
- Publisher
- American Geophysical Union (AGU)
- Published
- 2015-09-04
- Volume
- 42
- Issue
- 17
- Pages
- 7131-7138
- ISSN
- 0094-8276 (ISSN-L)
- 1944-8007
- OpenAlex
- W2112037160
- Cited by
- 93
- References
- 0
- Citations by year
- 2026: 8 · 2025: 12 · 2024: 13 · 2023: 12 · 2022: 4 · 2021: 8 · 2020: 10 · 2019: 9 · 2018: 8 · 2017: 6 · 2016: 3
- FWCI
- 4.72
- Type
- journal article
- Language
- en
- Open access
- bronze
- doi.org
- Locations
- Geophysical Research Letters (publishedVersion)
- Funders
- National Oceanic and Atmospheric Administration (NA14OAR4830103)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Oceanography › Oceanographic and Atmospheric Processes
- Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Tropical and Extratropical Cyclones Research
- Physical Sciences › Earth and Planetary Sciences › Oceanography › Ocean Waves and Remote Sensing
- Keywords
- tropical cyclones, upper ocean response, salinity effects, underwater gliders, coupled ocean-atmosphere model, tropical cyclone intensification, Puerto Rico
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