The Makassar Strait pycnocline variability at 20-40 days

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The characteristics and plausible genesis of the 20-40 day variability observed within the Labani Channel, a constriction within the Makassar Strait, Indonesia, are described. The 20-40 day variability, trapped beneath the depth of the strongest stratification of the pycnocline, is most evident in the across-strait flow, and in the across-strait gradient of the along-strait flow as well as in the vertical displacements of isotherms. The 20-40 day energy distribution of the across-strait flow is identifiable as a blue spectrum, demonstrating downward phase propagation. The flow fields are approximated by a vortex velocity structure, and the corresponding isotherm displacements imply potential vorticity conservation. We propose that the 20-40 day features observed in the Labani Channel are expressions of cyclonic and anti-cyclonic eddies that are advected southward within the Makassar Strait throughflow. Analysis of simulated eddy kinetic energy from an eddy-resolving model further indicates that the upstream instability of the background flow within Makassar Strait is the energy source for the eddies which are dissipated within the Labani Channel.

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