The Indonesian throughflow, its variability and centennial change
Author:
Publisher
Springer Science and Business Media LLC
Subject
General Earth and Planetary Sciences
Link
http://link.springer.com/article/10.1186/s40562-018-0102-2/fulltext.html
Reference74 articles.
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2. Cai W (2006) Antarctic ozone depletion causes an intensification of the Southern Ocean super-gyre circulation. Geophys Res Lett. https://doi.org/10.1029/2005GL024911
3. Clarke AJ, Liu X (1994) Interannual sea level in the northern and eastern Indian Ocean. J Phys Oceanogr 24:1224–1235. https://doi.org/10.1175/1520-0485(1994)024<1224:ISLITN>2.0.CO;2
4. Domingues CM, Maltrud ME, Wijffels SE et al (2007) Simulated Lagrangian pathways between the Leeuwin Current system and the upper-ocean circulation of the southeast Indian Ocean. Deep Res Part II 54:797–817. https://doi.org/10.1016/j.dsr2.2006.10.003
5. Du Y, Qu T (2010) Three inflow pathways of the Indonesian throughflow as seen from the simple ocean data assimilation. Dyn Atmos Oceans 50:233–256. https://doi.org/10.1016/j.dynatmoce.2010.04.001
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