1. Seasonal energy cycle of wind-driven ocean circulation with particular emphasis on the role of bottom topography
- Author
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Sakamoto, Toshihiro and Umetsu, Isao
- Subjects
Oceanographic research ,Continental margins ,Planetary science ,Energy transformation ,Ocean circulation ,Earth sciences - Abstract
To link to full-text access for this article, visit this link: http://dx.doi.org/10.1016/j.dsr.2005.09.004 Byline: Toshihiro Sakamoto (a), Isao Umetsu (a)(b) Abstract: We investigate how the bottom slope affects the time-dependent global energy balance of a two-layer subtropical gyre driven by seasonal winds in order to reformulate the concept joint effect of baroclinicity and bottom relief (JEBAR) based on energetics rather than vorticity dynamics. It is shown that the role of JEBAR in this situation is to transfer energy between the barotropic and baroclinic fields. Since a deep current tends to flow in meridional directions along a meridional ridge, the geostrophically balanced pressure-gradient forces can perform work on the zonal barotropic flow over the ridge. The direction of the deep motion, and hence the sign of the work is reversed seasonally because the pressure field in the lower layer exhibits an anticyclonic tendency in winter and a cyclonic tendency in summer. The topographic beta effect strengthens the work on the northwest and southeast sides of the ridge, so that the net contribution from the ridge region is negative in winter and positive in summer. On the other hand, this work must be canceled by enhancing the energy conversion to satisfy the energy equation. As a result, the ridge not only accelerates but also seasonally reverses the sign of the rate of energy conversion. With some modification, a meridional trench and a western continental slope turn out to have qualitatively the same effect on the seasonal transport variation. Therefore, the annual range in the barotropic transport of the gyre is, to varying degrees, reduced irrespective of the details of the large-scale bottom topography. Author Affiliation: (a) Department of Earth and Planetary Science, Graduate School of Science, The University of Tokyo, Tokyo 113-0033, Japan (b) Naval Systems Department, Radio Application Division, Aerospace and Defense Operations Unit, NEC Corporation, Fuchu, Tokyo 183-8501, Japan Article History: Received 17 February 2005; Revised 12 September 2005; Accepted 24 September 2005
- Published
- 2006