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Science 10 September 1993:
Vol. 261. no. 5127, pp. 1427 - 1431
DOI: 10.1126/science.261.5127.1427

Articles

Comparisons Between Seismic Earth Structures and Mantle Flow Models Based on Radial Correlation Functions

Thomas H. Jordan 1, Peter Puster 1, Gary A. Glatzmaier 2, and Paul J. Tackley 3

1 Department of Earth, Atmospheric, and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA 02139
2 Earth and Environmental Science Division and Institute of Geophysics and Planetary Physics, Los Alamos National Laboratory, Los Alamos, NM 87545
3 Seismological Laboratory, California Institute of Technology, Pasadena, CA 91125

Three-dimensional numerical simulations were conducted of mantle convection in which flow through the transition zone is impeded by either a strong chemical change or an endothermic phase change. The temperature fields obtained from these models display a well-defined minimum in the vertical correlation length at or near the radius where the barrier is imposed, even when the fields were filtered to low angular and radial resolutions. However, evidence for such a feature is lacking in the shear-velocity models derived by seismic tomography. This comparison suggests that any stratification induced by phase or chemical changes across the mid-mantle transition zone has a relatively small effect on the large-scale circulation of mantle material.

Submitted on May 6, 1993
Accepted on July 8, 1993


THIS ARTICLE HAS BEEN CITED BY OTHER ARTICLES:
Phase Boundaries and Mantle Convection.
J. E. Vidale, J. E. Vidale, and T. Lay (1993)
Science 261, 1401-1402
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Science. ISSN 0036-8075 (print), 1095-9203 (online)