The Mindanao and Halmahera Eddies—Twin Eddies Induced by Nonlinearities
- 1 December 2003
- journal article
- Published by American Meteorological Society in Journal of Physical Oceanography
- Vol. 33 (12), 2815-2830
- https://doi.org/10.1175/1520-0485(2003)033<2815:tmahee>2.0.co;2
Abstract
It is shown analytically that a nonlinear collision of northward- and southward-flowing western boundary currents (WBC) on a β plane produces both an anticyclonic and a cyclonic eddy. (On an f plane no eddies are established; similarly, no eddies are established in the linear limit.) The length scales of both the anticyclonic and cyclonic eddies are larger than most eddies in the ocean. Furthermore, the anticyclone scale is larger than the cyclone length scale because of the higher upstream momentum flux. A reduced-gravity numerical model is used to validate these analytical results. The balance of forces and the eddy size estimates (derived from the numerical simulations) agree with the analytical results. Based on the above collision problem, it is argued that the Halmahera and Mindanao eddies are required to balance the nonlinear momentum fluxes of their colliding parent currents, the southward-flowing Mindanao Current (MC) and the northward-flowing South Equatorial Current (SEC). Assuming that the interior is in Sverdrup balance, it is further argued that neither of the eddies would have been present had the Indonesian Throughflow not been active.Keywords
This publication has 30 references indexed in Scilit:
- Collision and separation of boundary currentsDeep Sea Research Part I: Oceanographic Research Papers, 1993
- Laminar separation of colliding western boundary currentsJournal of Marine Research, 1991
- A wind‐driven isopycnic coordinate model of the north and equatorial Atlantic Ocean: 1. Model development and supporting experimentsJournal of Geophysical Research: Oceans, 1990
- Recirculation and separation of boundary currentsJournal of Marine Research, 1990
- Wind‐driven spin‐up in eddy‐resolving ocean models formulated in isopycnic and isobaric coordinatesJournal of Geophysical Research: Oceans, 1986
- A Permanent Undercurrent Adjacent to the Great Barrier ReefJournal of Physical Oceanography, 1983
- Initial Testing of a Numerical Ocean Circulation Model Using a Hybrid (Quasi-Isopycnic) Vertical CoordinateJournal of Physical Oceanography, 1981
- The birth and death of a warm core ringJournal of Geophysical Research: Oceans, 1979
- Cross-equatorial inertial jets with special relevance to very remote forcing of the Somali CurrentDeep Sea Research Part A. Oceanographic Research Papers, 1979
- Computational design for long-term numerical integration of the equations of fluid motion: Two-dimensional incompressible flow. Part IJournal of Computational Physics, 1966