Indonesian throughflow nutrient fluxes and their potential impact on Indian Ocean productivity

TitleIndonesian throughflow nutrient fluxes and their potential impact on Indian Ocean productivity
Publication TypeJournal Article
Year of Publication2014
AuthorsAyers J.M, Strutton P.G, Coles V.J, Hood R.R, Matear R.J
JournalGeophysical Research Letters
Volume41
Pagination5060-5067
Date Published2014/07
Type of ArticleArticle
ISBN Number0094-8276
Accession NumberWOS:000340536000033
Keywordscirculation; enso; phosphate; seas; variability; waters
Abstract

The Indonesian throughflow (ITF) is a chokepoint in the upper ocean thermohaline circulation, carrying Pacific waters through the strongly mixed Indonesian Seas and into the Indian Ocean. Yet the influence of the ITF on biogeochemical fluxes into the Indian Ocean is largely unknown. This study determines the first depth-and time-resolved nitrate, phosphate, and silicate fluxes at the three main exit passages of the ITF:Lombok Strait, Ombai Strait, and Timor Passage. Nutrient flux as well as its variability with depth and time differs greatly between the passages. We estimate the effective flux of nutrients into the Indian Ocean by accounting for existing nutrients in the basin and find it largest in the upper 300-400 m. This suggests that the majority of ITF nutrient supply to the Indian Ocean is to thermocline waters, where it is likely to support new production and significantly impact Indian Ocean biogeochemical cycling.

DOI10.1002/2014gl060593
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