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- W3148997464 abstract "This paper describes for the first time the summer and winter distributions of sea surface δ13CDIC in the Southern Indian Ocean (20◦S–60◦S). For this we used δ13CDIC measurements from 10 cruises conducted between 1998 and 2005. For summer and winter, the highest δ 13 CDIC values (>2) are observed in sub-Antarctic waters (40 ◦ S–50 ◦ S) and attributed mainly to biological activity, enhanced in the vicinity of Crozet and Kerguelen Archipelagoes. The lowest δ 13 CDIC values are found in subtropical waters (25 ◦ S–35 ◦ S), with a minimum (<1) in the Agulhas Current region and in the Mozambique channel. On the seasonal scale, δ 13 CDIC is higher during summer than during winter in all regions. The largest seasonal amplitude of variation (∼0.3), observed in the region 35 ◦ S–40 ◦ S, is attributed to biological activity during summer and to deep vertical mixing during winter. In subtropical oligotrophic waters, the mean seasonal amplitude of variation (∼0.15) is mainly explained by air–sea CO2 fluxes. On the interannual scale, we also identified a large negative anomaly of δ 13 CDIC in the subtropical waters during austral summer 2002, associated to an anomalous ocean CO2 sink due to cold conditions during this period." @default.
- W3148997464 created "2021-04-13" @default.
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- W3148997464 date "2010-01-01" @default.
- W3148997464 modified "2023-09-27" @default.
- W3148997464 title "Summer and winter distribution of δ 13 C DIC in surface waters of the South Indian Ocean (20 ◦ S-60 ◦ S)" @default.
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