Analogies of Ocean/Atmosphere Rotating Fluid Dynamics with Gyroscopes: Teaching Opportunities

Thomas W. N. Haine Earth and Planetary Sciences, The Johns Hopkins University, Baltimore, Maryland

Search for other papers by Thomas W. N. Haine in
Current site
Google Scholar
PubMed
Close
and
Deepak A. Cherian Earth, Atmospheric, and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, Massachusetts

Search for other papers by Deepak A. Cherian in
Current site
Google Scholar
PubMed
Close
Restricted access

The dynamics of the rotating shallow-water (RSW) system include geostrophic f low and inertial oscillation. These classes of motion are ubiquitous in the ocean and atmosphere. They are often surprising to people at first because intuition about rotating f luids is uncommon, especially the counterintuitive effects of the Coriolis force. The gyroscope, or toy top, is a simple device whose dynamics are also surprising. It seems to defy gravity by not falling over, as long as it spins fast enough. The links and similarities between rotating rigid bodies, like gyroscopes, and rotating fluids are rarely considered or emphasized. In fact, the dynamics of the RSW system and the gyroscope are related in specific ways and they exhibit analogous motions. As such, gyroscopes provide important pedagogical opportunities for instruction, comparison, contrast, and demonstration. Gyroscopic precession is analogous to geostrophic flow and nutation is analogous to inertial oscillation. The geostrophic adjustment process in rotating fluids can be illustrated using a gyroscope that undergoes transient adjustment to steady precession from rest. The controlling role of the Rossby number on RSW dynamics is reflected in a corresponding nondimensional number for the gyroscope. The gyroscope can thus be used to illustrate RSW dynamics by providing a tangible system that behaves like rotating fluids do, such as the large-scale ocean and atmosphere. These relationships are explored for their potential use in educational settings to highlight the instruction, comparison, contrast, and demonstration of important fluid dynamics principles.

CORRESPONDING AUTHOR: Thomas W. N. Haine, 329 Olin Hall, The Johns Hopkins University, 3400 N. Charles St., Baltimore, MD 21218, E-mail: thomas.haine@jhu.edu

Supplements to this article are available online (10.1175/BAMS-D-12-00023.2 and 10.1175/BAMS-D-12-00023.3)

The dynamics of the rotating shallow-water (RSW) system include geostrophic f low and inertial oscillation. These classes of motion are ubiquitous in the ocean and atmosphere. They are often surprising to people at first because intuition about rotating f luids is uncommon, especially the counterintuitive effects of the Coriolis force. The gyroscope, or toy top, is a simple device whose dynamics are also surprising. It seems to defy gravity by not falling over, as long as it spins fast enough. The links and similarities between rotating rigid bodies, like gyroscopes, and rotating fluids are rarely considered or emphasized. In fact, the dynamics of the RSW system and the gyroscope are related in specific ways and they exhibit analogous motions. As such, gyroscopes provide important pedagogical opportunities for instruction, comparison, contrast, and demonstration. Gyroscopic precession is analogous to geostrophic flow and nutation is analogous to inertial oscillation. The geostrophic adjustment process in rotating fluids can be illustrated using a gyroscope that undergoes transient adjustment to steady precession from rest. The controlling role of the Rossby number on RSW dynamics is reflected in a corresponding nondimensional number for the gyroscope. The gyroscope can thus be used to illustrate RSW dynamics by providing a tangible system that behaves like rotating fluids do, such as the large-scale ocean and atmosphere. These relationships are explored for their potential use in educational settings to highlight the instruction, comparison, contrast, and demonstration of important fluid dynamics principles.

CORRESPONDING AUTHOR: Thomas W. N. Haine, 329 Olin Hall, The Johns Hopkins University, 3400 N. Charles St., Baltimore, MD 21218, E-mail: thomas.haine@jhu.edu

Supplements to this article are available online (10.1175/BAMS-D-12-00023.2 and 10.1175/BAMS-D-12-00023.3)

Supplementary Materials

    • Supplemental Materials (PDF 832.76 KB)
    • Supplemental Materials (PDF 129.43 MB)
Save
  • Barker, E. F., 1960: Elementary analysis of the gyroscope. Amer. J. Phys., 28, 808810.

  • Blackadar, A. K., 1957: Boundary layer wind maxima and their significance for the growth of nocturnal inversions. Bull. Amer. Meteor. Soc., 38, 283290.

    • Search Google Scholar
    • Export Citation
  • Brancazio, P. J., 1987: Rigid-body dynamics of a football. Amer. J. Phys., 55, 415420.

  • Butikov, E., 2006: Precession and nutation of a gyroscope. Eur. J. Phys., 27, 10711081.

  • Durran, D. R., 1993: Is the Coriolis force really responsible for the inertial oscillation? Bull. Amer. Meteor. Soc., 74, 21792184.

  • Durran, D. R., and S. K. Domonkos, 1996: An apparatus for demonstrating the inertial oscillation. Bull. Amer. Meteor. Soc., 77, 557559.

    • Search Google Scholar
    • Export Citation
  • Eastman, P. C., 1975: Painless precession. Amer. J. Phys., 43, 365366.

  • Edwards, P. L., 1977: A physical explanation of the gyroscope effect. Amer. J. Phys., 45, 11941195.

  • French, A. P., 1971: Newtonian Mechanics. W. W. Norton & Company, 743 pp.

  • Haken, H., 1975: Analogy between higher instabilities in fluids and lasers. Phys. Lett., 53A, 7778.

  • Haynes, P. H., and M. E. McIntyre, 1990: On the conservation and impermeability theorems for potential vorticity. J. Atmos. Sci., 47, 20212031.

    • Search Google Scholar
    • Export Citation
  • Haynes, P. H., C. J. Marks, M. E. McIntyre, T. G. Shepherd, and K. P. Shine, 1991: On the “downward control” of extratropical diabatic circulations by eddy-induced mean zonal forces. J. Atmos. Sci., 48, 651678.

    • Search Google Scholar
    • Export Citation
  • Illari, L., and Coauthors, 2009: “Weather in a Tank”— Exploiting laboratory experiments in the teaching of meteorology, oceanography, and climate. Bull. Amer. Meteor. Soc., 90, 16191632.

    • Search Google Scholar
    • Export Citation
  • Lock, J. A., 1989: An alternative approach to the teaching of rotational dynamics. Amer. J. Phys., 57, 428432.

  • Lorenz, E. N., 1963: Deterministic nonperiodic flow. J. Atmos. Sci., 20, 130141.

  • Lundquist, J. K., 2003: Intermittent and elliptical inertial oscillations in the atmospheric boundary layer. J. Atmos. Sci., 60, 26612673.

    • Search Google Scholar
    • Export Citation
  • Malkus, W. V. R., 1972: Non-periodic convection at high and low Prandtl number. Mem. Soc. Roy. Sci. Liege, 6, 125128.

  • Marshall, J. C., and R. A. Plumb, 2008: Atmosphere, Ocean, and Climate Dynamics: An Introductory Text. Elsevier, 319 pp.

  • Persson, A., 1998: How do we understand the Coriolis force? Bull. Amer. Meteor. Soc., 79, 13731385.

  • Phillips, N. A., 2000: An explication of the Coriolis effect. Bull. Amer. Meteor. Soc., 81, 299303.

  • Rasmussen, E. A., and J. Turner, 2003: Polar Lows: Mesoscale Weather Systems in the Polar Regions. Cambridge University Press, 612 pp.

  • Rhines, P. B., E. G. Lindahl, and A. J. Mendez, 2007: Optical altimetry: A new method for observing rotating f luids with applications to Rossby and inertial waves on a polar beta-plane. J. Fluid Mech., 572, 389412.

    • Search Google Scholar
    • Export Citation
  • Stommel, H. M., and D. W. Moore, 1989: An Introduction to the Coriolis Force. Columbia University Press, 297 pp.

  • Vallis, G. K., 1988: Conceptual model of El Niño and the Southern Oscillation. J. Geophys. Res., 93, 13 97913 991.

  • Vallis, G. K., 2006: Atmospheric and Oceanic Fluid Dynamics: Fundamentals and Large-Scale Circulation. Cambridge University Press, 745 pp.

    • Search Google Scholar
    • Export Citation
  • van Meurs, P., 1998: Interactions between near-inertial mixed layer currents and the mesoscale: The importance of spatial variabilities in the vorticity field. J. Phys. Oceanogr., 28, 13631388.

    • Search Google Scholar
    • Export Citation
All Time Past Year Past 30 Days
Abstract Views 0 0 0
Full Text Views 1126 468 35
PDF Downloads 747 221 23