Skip Navigation Links
Discontinuity, Nonlinearity, and Complexity

Dimitry Volchenkov (editor), Dumitru Baleanu (editor)

Dimitry Volchenkov(editor)

Mathematics & Statistics, Texas Tech University, 1108 Memorial Circle, Lubbock, TX 79409, USA

Email: dr.volchenkov@gmail.com

Dumitru Baleanu (editor)

Cankaya University, Ankara, Turkey; Institute of Space Sciences, Magurele-Bucharest, Romania

Email: dumitru.baleanu@gmail.com


Exact Solutions and Stability Analysis of a Nonlinear Model of Open-Ocean Deep Convection that Allows Multiple Steady States

Discontinuity, Nonlinearity, and Complexity 8(2) (2019) 169--186 | DOI:10.5890/DNC.2019.06.005

Igor L. Bashmachnikov$^{1}$,$^{2}$, DmitryV. Kovalevsky$^{3}$

$^{1}$ The Saint Petersburg State University, Department of Oceanography, Universitetskaya emb. 7-9, 199034 St. Petersburg, Russia

$^{2}$ Nansen International Environmental and Remote Sensing Centre, 14th Line 7, office 49, Vasilievsky Island, 199034 St. Petersburg, Russia

$^{3}$ Climate Service Center Germany (GERICS), Helmholtz-Zentrum Geesthacht, Fischertwiete 1, 20095 Hamburg, Germany

Download Full Text PDF

 

Abstract

We present analytical solutions of the two-basin model of open-ocean deep convection. Originally suggested by Whitehead [Whitehead, J.A. (2000), Stratified convection with multiple states, Ocean Modelling, 2(3-4), 109-121], the model allows regimes with multiple steady states (multiple equilibria). We provide the full analytical description of the steady states for the particular case of constant surface heat flux from the ocean to the atmosphere, and explore analytically stability of the equilibria within the Lyapunov theory. The results show that, for this particular case, the steady state is unique and stable for all dynamic flow regimes. We also present analytical expressions for dependence of critical values of sea-surface heat flux, at which transitions between the dynamic regimes occur, on the model parameters.

Acknowledgments

The research was supported by Russian Science Foundation – RSF (project No. 17-17-01151).

References

  1. [1]  Dijkstra, H.A. (2005), Nonlinear Physical Oceanography: A Dynamical Systems Approach to the Large-Scale Ocean Circulation and El Ni?no, 2nd ed., Kluwer Acad. Publishers: Dordrecht/Norwell, Mass.
  2. [2]  Ciani, D., Carton, X., Bashmachnikov, I., Chapron, B., and Perrot, X. (2015), Influence of deep vortices on the ocean surface, Discontinuity, Nonlinearity, and Complexity, 4(3), 281-311, DOI: 10.5890/DNC.2015.09.006.
  3. [3]  Volchenkov, D. (2010), Critical hydrodynamics: from turbulence to tsunami waves, to synaptic eddies, In: Turbulence: Theory, Types and Simulation, R.J. Marcuso (Ed.), 2010, Ch. 12, 407-478, NOVA Science Publishers, Inc., USA, ISBN: 978-1-61761-735-5.
  4. [4]  Arto, I., Capellán-Pérez, I., Filatova, T., González-Eguino, M., Hasselmann, K., Kovalevsky, D.V., Markandya, A., Moghayer, S.M., and Tariku, M.B. (2013), Review of existing literature on methodologies to model non-linearity, thresholds and irreversibility in high-impact climate change events in the presence of environmental tipping points. EU FP7 COMPLEX Report D5.2, 31 December 2013. URL: http://owsgip.itc.utwente.nl/projects/complex/complex files/COMPLEX Report D52 2013%2031%2012.pdf
  5. [5]  Chu, P.C. (1991), Geophysics of deep convection and deep water formation in oceans, In: Deep Convection and Deep Water Formation in the Oceans, P.C. Chu and J.C. Gascard (Eds.), Elsevier Oceanography Series, 57, 3-16.
  6. [6]  Marshall, J. and Schott, F. (1999), Open-ocean convection: Observations, theory, and models, Reviews of Geophysics, 37(1), 1-64, DOI: 10.1029/98RG02739.
  7. [7]  Alekseev, G.V., Johannessen, O.M., Korablev, A.A., Ivanov, V.V., and Kovalevsky, D.V. (2001), Interannual variability in water masses in the Greenland Sea and adjacent areas, Polar Research, 20(2), 201-208, DOI: 10.1111/j.1751- 8369.2001.tb00057.x.
  8. [8]  Alekseev, G.V., Johannessen, O.M., and Kovalevskii, D.V. (2001), Development of convectivemotions under the effect of local perturbations of sea-surface density, Izvestiya - Atmospheric and Ocean Physics, 37(3), 341-350.
  9. [9]  Nagurnyi, A.P., Bogorodskii, P.V., Popov, A.V., and Svyashchennikov, A.N. (1985), Intense formation of cold bottom waters on the Greenland Sea surface, Transactions (Doklady) of the USSR Academy of Sciences, 284(2), 478 (in Russian).
  10. [10]  Johannessen, O.M., Sandven, S., and Johannessen, J.A. (1991), Eddy-related winter convection in the Boreas Basin, In: Deep Convection and Deep Water Formation in the Oceans, P.C. Chu and J.C. Gascard (Eds.), Elsevier Oceanography Series, 57, 87-105.
  11. [11]  Dickson, R.R., Osborn, T.J., Hurrell, J.W., Meincke, J., Blindheim, J., Adlandsvik, B., Vinje, T., Alekseev, G., and Maslowski,W. (2000), The Arctic Ocean response to the North Atlantic Oscillation, Journal of Climate, 13(15), 2671- 2696.
  12. [12]  Buckley, M.W. andMarshall, J. (2016), Observations, inferences, and mechanisms of Atlantic Meridional Overturning Circulation variability: A review, Reviews of Geophysics, 54, 5-63, DOI: 10.1002/2015RG000493.
  13. [13]  Cuffey, K.M. and Clow, G.D. (1997), Temperature, accumulation, and ice sheet elevation in central Greenland through the last deglacial transition, Journal of Geophysical Research, 102, 26383-26396, DOI: 10.1029/96JC03981.
  14. [14]  Broecker, W.S. (1998), Paleocean circulation during the last deglaciation: A bipolar seesaw? Paleoceanography, 13, 119-121, DOI: 10.1029/97PA03707.
  15. [15]  Androsov, A., Rubino, A., Romeiser, R., and Sein, D.V. (2005), Open-ocean convection in the Greenland Sea: preconditioning through a mesoscale chimney and detectability in SAR imagery studied with a hierarchy of nested numerical models, Meteorologische Zeitschrift, 14(6), 693-702, DOI: 10.1127/0941-2948/2005/0078.
  16. [16]  Brugge, R., Jones, H.L., and Marshall, J.C. (1991), Non-hydrostatic ocean modelling for studies of open-ocean deep convection. In: Deep Convection and Deep Water Formation in the Oceans, P.C. Chu and J.C. Gascard (Eds.), Elsevier Oceanography Series, 57, 325-340.
  17. [17]  Mikolajewicz, U., Sein, D.V., Jacob, D., Königk, T., Podzun, R., and Semmler, T. (2005), Simulating Arctic sea ice variability with a coupled regional atmosphere-ocean-sea ice model, Meteorologische Zeitschrift, 14(6), 793-800, DOI: 10.1127/0941-2948/2005/0083.
  18. [18]  Moore, G.W.K., Våge, K., Pickart, R.S., and Renfrew, I.A. (2015), Decreasing intensity of open-ocean convection in the Greenland and Iceland seas, Nature Climate Change, 5(9), 877, DOI: 10.1038/nclimate2688.
  19. [19]  Stommel, H. (1961), Thermohaline convection with two stable regimes of flow, Tellus, 13(2), 224-230.
  20. [20]  Stommel, H.M. and Young, W.R. (1993), The average T-S relation of a stochastically forced box model, Journal of Physical Oceanography, 23(1), 151-158.
  21. [21]  Cessi, P. (1994), A simple box model of stochastically forced thermohaline flow, Journal of Physical Oceanography, 24(9), 1911-1920.
  22. [22]  Scott, J.R., Marotzke, J., and Stone, P.H. (1999), Interhemispheric thermohaline circulation in a coupled box model, Journal of Physical Oceanography, 1999, 29(3), 351-365.
  23. [23]  Zickfeld, K., Slawig, T., and Rahmstorf, S. (2004), A low-order model for the response of the Atlantic thermohaline circulation to climate change, Ocean Dynamics, 54(1), 8-26, DOI: 10.1007/s10236-003-0054-7.
  24. [24]  Whitehead, J.A. (2000), Stratified convection with multiple states, Ocean Modelling, 2(3-4), 109-121, https://doi.org/10.1016/S1463-5003(00)00012-3.
  25. [25]  Garwood, R.W. (1991), Enhancements to deep turbulent entrainment, In: Deep Convection and Deep Water Formation in the Oceans, P.C. Chu and J.C. Gascard (Eds.), Elsevier Oceanography Series, 57, 197-213.
  26. [26]  Killworth, P.D. (1979), On "chimney" formations in the ocean, Journal of Physical Oceanography, 9(3), 531-554.
  27. [27]  Whitehead, J.A., Te Raa, L., Tozuka, T., Keller, J.B., and Bradley, K. (2005), Laboratory observations and simple models of slow oscillations in cooled salt-stratified bodies, Tellus A: Dynamic Meteorology and Oceanography, 57(5), 798-809, http://dx.doi.org/10.3402/tellusa.v57i5.14739.
  28. [28]  Whitehead, J.A. and Bradley, K. (2006), Laboratory studies of stratified convection with multiple states, Ocean Modelling, 11(3-4), 333-346, https://doi.org/10.1016/j.ocemod.2005.01.002.
  29. [29]  Whitehead, J.A. (2009), Abrupt transitions and hysteresis in thermohaline laboratory models, Journal of Physical Oceanography, 39(5), 1231-1243, DOI: 10.1175/2008JPO4087.1.
  30. [30]  Kundu, P.K., Cohen, I.M., and Dowling, D.R. (2012), Fluid Mechanics, 5th ed., Academic Press: Boston.
  31. [31]  Kamke, E. (1959), Differentialgleichungen: Lösungsmethoden und Lösungen. I. Gewöhnliche Differentialgleichungen.[Differential Equations: Solution Methods and Solutions. I. Ordinary differential equations.] 6. verbesserte Auflage, Leipzig.