Skip to main content
Log in

The influence of Gulf of Mexico Loop Current intrusion on the transport of the Florida Current

  • Published:
Ocean Dynamics Aims and scope Submit manuscript

Abstract

Based on an empirical orthogonal function analysis of satellite altimeter data, guidance from numerical model results, and CANEK transport estimates, we propose an index, based on differences in satellite-measured sea surface height anomalies, for measuring the influence of Gulf of Mexico Loop Current intrusion on vertically integrated transport variability through the Yucatan Channel. We show that the new index is significantly correlated at low frequencies (cut-off 120 days) with the cable estimates of transport between Florida and the Bahamas. We argue that the physical basis for the correlation is the geometric connectivity between the Yucatan Channel and the Straits of Florida.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Fig. 1
Fig. 2
Fig. 3
Fig. 4
Fig. 5
Fig. 6
Fig. 7

Similar content being viewed by others

References

  • Anderson DLT, Corry RA (1985) Seasonal transport variations in the Florida Straits: a model study. J Phys Oceanogr 15:773–786

    Article  Google Scholar 

  • Baringer MO, Larsen JC (2001) Sixteen years of Florida Current transport at 27˚N. Geophys Res Lett 28:3179–3182

    Article  Google Scholar 

  • Beal LM, Hummon JM, Williams E, Brown OT, Baringer W, Kearns EJ (2008) Five years of Florida Current structure and transport from the Royal Caribbean cruise ship “Explorer of the Seas”. J Geophys Res 113:C06001. doi:10.1029/2007JC004154

    Article  Google Scholar 

  • Bunge L, Ochoa J, Badan A, Candela J, Sheinbaum J (2002) Deep flows in the Yucatan Channel and their relation to changes in the loop current extension. J Geophys Res 107:3233. doi:10.1029/2001JC001256

    Article  Google Scholar 

  • Cherubin LM, Sturges W, Chassignet EP (2005) Deep flow variability in the vicinity of the Yucatan Straits from a high-resolution numerical simulation. J Geophys Res 110:C04009. doi:10.1029/2004JC002280

    Article  Google Scholar 

  • Cunningham, S. A., T. Kanzow, D. Rayner, et al., 2007: Temporal variability of the Atlantic Meridional Overturning Circulation at 26.5°N, Science, 317, 935–938.

    Google Scholar 

  • DiNezio PN, Clement AC, Vecchi GA, Soden BJ, Kirtman BP et al (2009) Climate response of the equatorial Pacific to global warming. J Clim 22:4873–4892

    Article  Google Scholar 

  • Eden C, Greatbatch RJ, Willebrand J (2007) A diagnosis of thickness fluxes in an eddy-resolving model. J Phys Oceanogr 37(S.):727–742

    Article  Google Scholar 

  • Ezer T, Oey L-Y, Sturges W, Lee H-C (2003) The variability of currents in the Yucatan Channel: analysis of results from a numerical ocean model. J Geophys Res 108:3012. doi:10.1029/2002JC001509

    Article  Google Scholar 

  • Fanning AF, Greatbatch RJ, Da Silva AM, Levitus S (1994) Model-calculated seasonal transport variations through the Florida Straits: a comparison using different wind-stress climatologies. J Phys Oceanogr 24:30–45

    Article  Google Scholar 

  • Gill AE, Niiler PP (1973) The theory of the seasonal variability in the ocean. Deep Sea Res 20:141–177

    Google Scholar 

  • Greatbatch RJ, Goulding A (1989) Seasonal variations in a linear barotropic model of the North Atlantic driven by the Hellerman and Rosenstein wind stress field. J Phys Oceanogr 94:12645–12665

    Google Scholar 

  • Greatbatch RJ, Lu Y, deYoung B, Larsen J (1995) The variation of transport through the Straits of Florida: a barotropic model study. J Phys Oceanogr 25:2726–2740

    Article  Google Scholar 

  • Hamilton P, Larsen JC, Leaman KD, Lee TN, Waddell E (2005) Transports through the Straits of Florida. J Phys Oceanogr 35:308–322

    Article  Google Scholar 

  • Huh OK, Wiseman WJ, Rouse LJ (1981) Intrusion of Loop Current waters onto the West Florida continental shelf. J Geophys Res 86:4186–4192

    Article  Google Scholar 

  • Hurlburt HE, Thompson JD (1980) A numerical study of Loop Current intrusions and eddy shedding. J Phys Oceanogr 10:1611–1651

    Article  Google Scholar 

  • Kanzow T, Cunningham SA, Rayner D, Hirschi JJ-M, Johns WE et al (2007) Observed flow compensation associated with the MOC at 26.5°N in the Atlantic. Science 317:938–941

    Article  Google Scholar 

  • Larsen JC (1992) Transport and heat flux of the Florida Current at 27°N derived from cross-stream voltages and profiling data: theory and observations. Philos Trans R Soc Lond 338:169–236

    Article  Google Scholar 

  • Le Traon PY, Nadal F, Ducet N (1998) An improved mapping method of multi-satellite altimeter data. J Atmos Ocean Technol 25:522–534

    Article  Google Scholar 

  • Lin Y, Greatbatch RJ, Sheng J (2009) A model study of the vertically integrated transport variability through the Yucatan Channel: role of Loop Current evolution and flow compensation around Cuba. J Geophys Res 114:C08003. doi:10.1029/2008JC005199

    Article  Google Scholar 

  • Maul GA, Vukovich FM (1993) The relationship between variations in the Gulf of Mexico loop current and Straits of Florida volume transport. J Phys Oceanogr 23:785–796

    Article  Google Scholar 

  • Niiler PP, Richardson WS (1973) Seasonal variability of the Florida Current. J Mar Res 31:144–166

    Google Scholar 

  • Ochoa J, Sheinbaum J, Badan A, Candela J, Wilson D (2001) Geostrophy via potential vorticity inversion in the Yucatan Channel. J Mar Res 59:725–747

    Article  Google Scholar 

  • Oey L-Y, Lee H, Schmitz WJ Jr (2003) Effects of winds and Caribbean eddies on the frequency of loop current eddy shedding: a numerical model study. J Geophys Res 108:3324

    Article  Google Scholar 

  • Oey, L.-Y., T. Ezer, and H.-C. Lee, 2005: Loop Current, rings and related circulation in the Gulf of Mexico: a review of numerical models and future challenges, in Circulation in the Gulf of Mexico: Observations and Models, Geophys. Monograph Ser., 161, W. Sturges and A. Lugo-Fernandez, Eds., 360 pp., AGU, Washington, D. C.

  • Schmitz WJ, Richardson PL (1991) On the sources of the Florida Current. Deep Sea Res 32:S379–S409

    Google Scholar 

  • Schmitz WJ Jr, Thompson JD, Luyten JR (1992) Sverdrup circulation for the Atlantic along 24°N. J Geophys Res 97:7251–7256

    Article  Google Scholar 

  • Schott F, Zantopp R (1985) Florida current: seasonal and interannual variability. Science 227:308–311

    Article  Google Scholar 

  • Sheinbaum J, Candela J, Badan A, Ochoa J (2002) Flow structure and transport in the Yucatan channel. Geophys Res Lett 29:1040. doi:10.1029/2001GL013990

    Article  Google Scholar 

  • Sturges W, Leben R (2000) Frequency of ring separations from the loop current in the Gulf of Mexico: a revised estimate. J Phys Oceanogr 30:1814–1819

    Article  Google Scholar 

  • Vukovich FM (1995) An updated evaluation of the loop current’s eddy-shedding frequency. J Geophys Res 100:8655–8659

    Article  Google Scholar 

  • Wiseman WJ Jr, Dinnel SP (1988) Shelf currents near the mouth of the Mississippi River. J Phys Oceanogr 18:1287–1291

    Article  Google Scholar 

Download references

Acknowledgments

The authors wish to thank Julio Sheinbaum for providing the observations taken during the CANEK program and Lisa Beal for providing the transport estimates from the “Explorer of the Seas” data set. Comments from two reviewers led to improvements in the manuscript and are acknowledged. This work has been funded by the NSERC/MARTEC/EC Industrial Research Chair awarded to RJG and JS as well as support to RJG from IFM-GEOMAR.

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Yuehua Lin.

Additional information

Responsible Editor: John Wilkin

Rights and permissions

Reprints and permissions

About this article

Cite this article

Lin, Y., Greatbatch, R.J. & Sheng, J. The influence of Gulf of Mexico Loop Current intrusion on the transport of the Florida Current. Ocean Dynamics 60, 1075–1084 (2010). https://doi.org/10.1007/s10236-010-0308-0

Download citation

  • Received:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1007/s10236-010-0308-0

Keywords

Navigation