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Detailed Reference Information |
Stewart, C.A. (1992). Thermal convection in the Earth's mantle: Mode coupling induced by temperature-dependent viscosity in a three-dimensional spherical shell. Geophysical Research Letters 19: doi: 10.1029/92GL00163. issn: 0094-8276. |
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Temperature-dependent viscosity places constraints on the spherical harmonic spectrum of thermal convection in the earth's mantle. Viscosity, being a strong function of temperature, gives rise to quantized feed-back loops among low-order modes in the governing equations. This nonlinear resonance is proposed as the cause of the dominance of a low-order convective pattern in the earth's mantle. ¿ American Geophysical Union 1992 |
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BACKGROUND DATA FILES |
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Abstract![](/images/icons/spacer.gif) |
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Keywords
Tectonophysics, Dynamics of the lithosphere and mantle, Tectonophysics, Rheology of the lithosphere and mantle, Planetology, Solid Surface Planets and Satellites, Interiors, Planetology, Solid Surface Planets and Satellites, Tectonics |
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Publisher
American Geophysical Union 2000 Florida Avenue N.W. Washington, D.C. 20009-1277 USA 1-202-462-6900 1-202-328-0566 service@agu.org |
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