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Instability caused by the coalescence of two modes of a one-layer coastal current with a surface front

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Abstract

Stability of a one-layer density-driven coastal current with a surface front whose potential vorticity is uniformly zero is examined, and it is shown that such a current can be unstable if the stability condition derived by Paldor (1983) is not satisfied,i.e., the current width,L, is larger than 2/3U/f, wheref is the Coriolis parameter andU is the current velocity at the front. This instability is caused by the coalescence of a frontal trapped and coastal trapped waves. The energetics of this instability and the effect of potential vorticity gradient are also discussed.

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References

  • Cairns, R.A. (1979): The role of negative energy waves in some instabilities of parallel flows. J. Fluid Mech.,92, 1–14.

    Article  Google Scholar 

  • Eady, E.T. (1949): Long waves and cyclone waves. Tellus,1, 33–52.

    Article  Google Scholar 

  • Griffiths, R.W., P.D. Killworth and M.E. Stern (1982): Ageostrophic instability of ocean currents. J. Fluid Mech.,117, 343–377.

    Article  Google Scholar 

  • Killworth, P. D. (1983): Long-wave instability of an isolated front. Geophys. Astrophys. Fluid Dyn.,25, 235–258.

    Article  Google Scholar 

  • Killworth, P.D. and M.E. Stern (1982): Instabilities on density driven boundary currents and fronts. Geophys. Astrophys. Fluid Dyn.,22, 1–28.

    Article  Google Scholar 

  • Killworth, P.D., N. Paldor and M.E. Stern (1984): Wave propagation and growth on a surface front in a two-layer geostrophic current. J. Mar. Res.,42, 761–785.

    Article  Google Scholar 

  • Kubokawa, A. (1985): Instability of a geostrophic front and its energetics. Geophys. Astrophys. Fluid Dyn.,33, 223–257.

    Article  Google Scholar 

  • Kubokawa, A. and K. Hanawa (1984): A theory of semigeostrophic gravity waves and its application to the intrusion of a density current along a coast. Part 1. J. Oceanogr. Soc. Japan,40, 247–259.

    Article  Google Scholar 

  • Legeckis, R. (1978): A survey of worldwide sea surface temperature fronts detected by environmental satellites. J. Geophys. Res.,83, 4501–4522.

    Article  Google Scholar 

  • Mechoso, C.R. and D.M. Sinton (1983): On the energy analysis of two layer frontal model. J. Atmos. Sci.,40, 2069–2074.

    Article  Google Scholar 

  • Orlanski, I. (1968): Instability of frontal waves. J. Atmos. Sci.,25, 178–200.

    Article  Google Scholar 

  • Paldor, N. (1983): Stability and stable modes of coastal fronts. Geophys. Astrophys. Fluid Dyn.,27, 217–228.

    Article  Google Scholar 

  • Ramp, S.R., R.C. Beardsley and R. Legeckis (1983): An observation of frontal wave development on a shelf-slope/warm core ring front near the shelf break south of New-England. J. Phys. Oceanogr.,13, 907–912.

    Article  Google Scholar 

  • Stern, M.E. (1980): Geostrophic front, bore, breaking and blocking waves. J. Fluid Mech.,99, 687–703.

    Article  Google Scholar 

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Kubokawa, A. Instability caused by the coalescence of two modes of a one-layer coastal current with a surface front. J Oceanogr 42, 373–380 (1986). https://doi.org/10.1007/BF02110432

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  • DOI: https://doi.org/10.1007/BF02110432

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