Abstract The Indian Ocean presents two distinct climate regimes. The north Indian Ocean is
dominated by the monsoons, whereas the seasonal reversal is less pronounced in the …

A review is presented of the ocean circulation along Australia's southern shelves and slope.
Uniquely, the long, zonal shelf is subject to an equatorward Sverdrup transport that gives …

Globally, rivers deliver significant quantities of nitrogen (N) and phosphorus (P) to the
coastal ocean each year. Currently, there are no viable estimates of how much of this N and …

Abstract Changes in coastal upwelling strength have been widely studied since 1990 when
Bakunproposed that global warming can induce the intensification of upwelling in …

Although the dominant boundary current off Western Australia is the poleward-flowing
Leeuwin Current, satellite imagery shows that there is a cool equatorward coastal …

Ferromanganese crusts provide records of long term change in ocean circulation and
continental weathering. However, calibrating their age prior to 10 Ma has been entirely …

Monsoon forcing and the unique geomorphology of the Indian Ocean basin result in
complex boundary currents, which are unique in many respects. In the northern Indian …

The seasonal cycle of physical, chemical, and biological properties of the surface ocean
mixed layer in the Australasian region (0 to 50° S, 90 to 180° E) were described on the basis …

The southwestern continental margin of Australia (19 degrees S-22 degrees S) in the
western Indian Ocean is transitional between cool-water and warm-water carbonate realms …

A~ 60 yr physical and chemical data set from 4 coastal stations around Australia plus
remotely sensed SeaWiFS and phytoplankton taxonomic data were used to evaluate the …