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For the last 20 years, much of my research has been directed at the ~10 percent of the equatorial circumference represented by the Indonesian seas. To understand my entry into Indonesian oceanography,...
In recent years there has been a marked advance in our understanding of Indonesian seas oceanography. This progress is a result of the growing interest of the oceanographic community in the unique cha...
Baroclinic, or internal, tides play a significant role in mixing in the deep ocean and in shallow seas (Munk and Wunsch, 1998; Garrett, 2003). In a stratified ocean, when the vertically uniform horizo...
The Indonesian throughflow (ITF) is the flow of warm, relatively fresh waters into the southeast Indian Ocean from the western Pacific Ocean via the series of passages between the islands of the Indon...
Tidal phenomena in the Indonesian seas are among the most complex in the world. Complicated coastal geometries with narrow straits and myriad small islands, rugged bottom topography next to wide shelv...
The global ocean is composed of parts—its regionseach playing a role in the global scheme of the ocean and climate systems. Each region has its intrinsic interest and uniqueness. Of course, the same ...
The Indonesian seas contain evidence of enhanced vertical mixing. Coupled with the highly stratified tropical thermocline, this enhanced mixing implies large vertical fluxes of heat and buoyancy from ...
Expressions of low-frequency tidal periods are found throughout the Indonesian Seas' temperature field, supporting the hypothesis that vertical mixing is enhanced within the Indonesian Seas by the tid...
Intraseasonal oscillations in sea level, sea surface temperature, and upper ocean flow field have recently been observed in various locations surrounding the Indonesian seas. While the observed oscill...
The Indonesian Throughflow, weaving through complex topography, drawing water from near the division of the North Pacific and South Pacific water mass fields, represents a severe challenge to modeling...

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