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New Zealand is the most oceanic nation of significant size, in the world's largest ocean. It is more than 1600 km from the nearest continent, has a land area of 268,200 km2 (103,552 square miles), and...
Biological communities are changing drastically in response to global climate change (Walther et al., 2002), changes in use by human populations (Krishtalka et al., 2002), and introduction of exotic s...
During the inaugural Physical Oceanography Dissertation Symposium in June 2002 we found that the graduate school experience varied markedly amongst the 20 international participants. The diversity of ...
In addition to providing financial support for much of the oceanographic research conducted at universities and research institutions in the U.S., the National Science Foundation (NSF) supports much o...
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...
Intrathermocline eddies (ITEs) are characterized by a subsurface lens of relatively homogeneous water. By definition, they are situated within the thermocline and therefore split the stratified water ...
The present-day assessment of contributions to sea level rise from glaciers and ice sheets depends to a large degree on new technologies that allow efficient and precise detection of change in otherwi...
As the only United Nations organization specializing in ocean sciences, the Intergovernmental Oceanographic Commission (IOC) has the responsibility to promote basic marine scientific investigations gl...
We used amino acid (AA) compound-specific isotope analysis (d15NAA and d13 CAA values) of midwater zooplankton and suspended particles to examine their dynamics in the mesopelagic zone. Suspended pa...
A simple point-vortex “heton” model is used to study localized ocean convection. In particular, the statistically steady state that is established when lateral buoyancy transfer, effected by baroclini...
A different way of looking at the meridional warm water (σθ < 26.8) flux in the South and North Atlantic is proposed. The approach involves the blending of observational aspects into analytical modeli...
In April 1961, 13.5 m of basalts were drilled off Guadalupe Island about 240 km west of Mexico's Baja California, together with a few hundred meters of Miocene sediments, in about 3500 m of water. Thi...

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