Tim Rixen

TL;DR: In this article, the authors present total and bulk component fluxes measured for 3 years at the central station and for 4 years at different locations in the western and eastern stations of the Arabian Sea, showing that more than 50% of the annual particle fluxes to the deep sea occur during the SW monsoon at the western location due to the prolonged influence of the monsoonal upwelling.

TL;DR: Dauwe et al. as discussed by the authors found that δ15N minima in the northern Bay of Bengal are caused by input of terrestrial organic matter as well as depleted nitrate from rivers.

TL;DR: In this article, the authors present estimates of various sources and sinks such as atmospheric dry and wet depositions of N aerosols, pelagic denitrification, nitrous oxide (N2O) emissions, and advective N input from the south.

TL;DR: In this article, sources and discharges of dissolved organic carbon (DOC) from the central Sumatran river Siak were studied and it was estimated that the DOC input from the Siak into the ocean was estimated to be ∼0.3 Tg C−1.

TL;DR: The results from sediment trap experiments conducted in the seasonal upwelling area off south Java from November 2000 until July 2003 revealed significant monsoon-, El Nino-Southern Oscillation and Indian Ocean Dipole-induced seasonal and interannual variations in flux and shell geochemistry of planktonic foraminifera as discussed by the authors.