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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...
In the New Zealand fjords, hydrogen sulfide production from decomposing forest litter is used by chemoautotrophs to fix CO2[aq]and support benthic food webs. We used quantitative surveys and stable is...
A steady-state model of the ocean circulation applied to an ocean area surrounding New Zealand, driven by specified density and wind stress distributions and specified flow at the boundaries of the oc...
A long term wave recording program based on the west coast of New Zealand has allowed a number of fundamental properties of the ocean-wave field to be studied. This paper deals with wave-generation pr...
The coastal ocean response to wind forcing on the west coast continental shelf of South Island, New Zealand is examined using current, sea level and wind observations. Weather band motions over the no...
Variations in coastal sea level in the weather band (periods 5–20 days) on the west coat of New Zealand can largely be explained in terms of wind-forced coastal-trapped waves. Long-wave theory was app...
Separate one-month current meter deployments in 1996 and 1997 over the Chatham Rise, east of New Zealand, show that tidal phases are both stable in time and close to those derived from a barotropic ti...
The Southland Current is a western boundary current adjacent to the South Island of New Zealand and flows along a segment of the Southern Hemisphere subtropical front (STF). The physical mechanisms th...
Patterns in morphology, pigment concentration, and light saturation kinetics of Ecklonia radiata reveal great morphological and physiological variability among individuals from sites spanning strong ...

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