The Kuroshio edge exchange processes (KEEP) study - an introduction to hypotheses and highlights

The Kuroshio edge exchange processes (KEEP) study is a multidisciplinary st udy on the internal cycling of material, especially carbon, within the East China Sea Shelf and the exchange of material between this Shelf and its ad joining Kuroshio. The project has been ongoing since 1989. The East China S ea Shelf is a net sink of atmospheric carbon dioxide. Rich supplies of nutr ients. mostly from the upwelling of the Kuroshio Subsurface Water and, to a lesser extent, from the riverine discharges, notably from the Changjiang, sustain a high primary production (550 mg C m(-2) d(-1)) on the Shelf and h elp the draw down of carbon dioxide. The sum of the demands for organic car bon for sustaining the observed bacterial production in the water column an d the rate of sulfate reduction in the sediments of this Shelf appears to e xceed its primary production. This suggests that a large fraction of the ph otosynthetically fixed carbon is recycled effectively within the Shelf. How ever, a comprehensive and definitive carbon budget for the Shelf cannot yet be constructed. Organic particles that survive oxidation within the Shelf and reach the Okinawa Trough are deposited in a belt along the upper northw estern slope of the Trough. A particle-rich mid-depth layer and the very hi gh fluxes of sinking particles off the shelf break northeast of Taiwan sugg est active cross shelf transport of particles from the Shelf to the Okinawa Trough. The cyclonic eddy at the shelf edge northeast of Taiwan is an impo rtant pathway for the exchange of dissolved and particulate materials betwe en the Shelf and the Kuroshio. Nitrogen fixation may be a significant contr ibutor of combined nitrogen to the oligotrophic Kuroshio Surface Water and the Taiwan Strait Warm Water so that it may support up to 25% of the new pr oduction in the Kuroshio Surface Water. (C) 2000 Elsevier Science Ltd. All rights reserved.