Relating Geophysical Structures and Processes: The Jeffreys by Keiiti Aki, Renata Dmowska

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By Keiiti Aki, Renata Dmowska

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Published through the yankee Geophysical Union as a part of the Geophysical Monograph Series.


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And H. Riehl, On the dynamics and energy transformations in steady-state hurricanes. Teflur,12. 1-20. 1960. Miller. L. On the maximum intensity of humcanes, J. , 15, 184195, 1958. Ooyama, K.. On the stability of the baroclinic circular vortex: a sufficient criterion for instability, J. A t m . 1966. , Numerical simulation of the life cycle of tropical cyclones, J. Atmos. 3-40, 1969a. 4,1968, Japan Meteorological Agency, Tokyo, 1969b. Pfeffer. R. , and M. Challa, A numerical study of the role of eddy fluxes of momentum in the development of Atlantic hurricanes, J.

J a p n , 44,353-375, 1966. Tuleya. R. E.. Sensitivity studies of tropical storm genesis using a numerical model, Mon. , 119,721-733, 1991. Tuleya, R. , and Y. Kurihara, A n~lmericalstudy of the effects of environmental flow on tropical storm genesis, Mon. Wea. , 109, 2487-2506, 1981. Tuleya, R. , M. A. Bender, and Y. Kurihara, A simulation study of the landfall of tropical cyclones using a movable nested-mesh model, Mon. Wea. , 112, 124-136, 1984. Willoughby, H. , Gradient balance in tropical cyclones, J.

Figure 2 (upper part) shows the flexural uplift of the ocean ridge and the deviatoric stress in the upper elastic part of the lithosphere for Model RIG2 of a normal oceanic ridge as described above. An enlarged plot of the central region is shown below the main model. The deviatoric stress has been concentrated into the upper elastic part of the lithosphere. Small tensions occur near the ridge crest as a result of the ongoing extension, representing the ridge resistance. These give way laterally a t about 40 krn to horizontal deviatoric compressions which increase t o about 40 MPa a t about 200 km from the ridge crest, remaining a t about this level out to the oldest ocean floor because of trade-off between increasing tectonic force and thickening elastic layer.

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