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The tropical ocean spans 82 percent of Earth's equatorial circumference (Indonesian maritime continent included). Here, where the atmosphere's opposing Hadley Cells meet to produce the rainy Intertrop...
Carbon (C) and alkalinity export from two adjacent intertidal inlets with different terrestrial inputs was investigated. One inlet receives a small creek from an agriculturally dominated catchment, l...
Hypoxia and anoxia in coastal waters have typically been explained by the respiration of sinking organic matter associated with nutrient over-enrichment and phytoplankton blooms. Here, we assess wheth...
Hypoxia and anoxia in coastal waters have typically been explained by the respiration of sinking organic matter associated with nutrient over-enrichment and phytoplankton blooms. Here, we assess wheth...
Low-salinity water masses were occasionally observed in spring and summer on the surface of the Kuroshio, south of Japan. Many of the masses were accompanied by excessive discharge of fresh water from...
The renewal of oxygen-rich water in the deep basins of the Baltic Sea depends mainly on the proper wind conditions. Strong westerly winds over the western Baltic yield an inclination in sea level from...
Experiments with an oceanic general circulation model indicate that the tropical and subtropical oceanic circulations are linked in three ways. Far from coast in the oceanic interior, equatorial surfa...
The authors examine the effect of fortnightly modulated tidal mixing over a sill on a bidirectional estuarine shear flow through it. The study proceeds numerically by using two sets of vertically two-...
The effect of meridional movement of the curl τ = 0 line on the intergyre transport is investigated by passive tracer experiments in a double gyre circulation. Furthermore, the contribution to tempera...
A numerical model is used to simulate deep water renewals that were observed to occur in Burrard Inlet/Indian Arm over a time period of about 100 days during winter 1984/85. The renewals (bottom water...
We conducted four field campaigns to evaluate benthic O2 consumption and the effect of advective pore-water flow in nearshore permeable sediments in the North Sea and Baltic Sea. Advective pore-wate...
Ballast water is a major vector of nonindigenous species invasion globally. Mandatory ballast water exchange (BWE) was implemented for vessels carrying ballast water into the Great Lakes in 1993. Desp...
Five field trips were conducted in the San Francisco Bay–Delta between May 2000 and October 2001 to investigate the sediment–water exchange of total mercury (Hg) and monomethyl mercury (MMHg). S...
The effects of advective pore water exchange driven by shallow water waves on the oxygen distribution in a permeable (k = 3.3 x 10-12 to 4.9 x 10-11 m2) natural sediment were studied with a planar oxy...
The effects of surface gravity waves on pore-water release from permeable sediment (k 5 1.3–1.8 3 10211 m2 ) in shallow water were studied in a wave tank. Our tracer experiments demonstrated that s...

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