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the claim

Ocean currents and wind stress generate odd-looking current patterns in the Tasman Sea

the verdict
SUPPORTED
the evidence backs this
Recorded sources
3 sources for · 0 against

Counts group repeated records of the same source within each side. They do not measure evidence strength or source independence.

Evidence confirms that wind stress and ocean currents, such as the East Australian Current, interact to create complex circulation and eddy patterns in the Tasman Sea.

The analysis

The retrieved papers specifically discuss the East Australian Current, wind stress variability, eddy shedding, and complex regional circulation patterns in the Tasman Sea, strongly supporting the claim.

Evidence for · 3
Recorded source metadata

Oliver ECJ, Benthuysen JA, Bindoff NL, Hobday AJ, Holbrook NJ, Mundy CN, Perkins-Kirkpatrick SE. The unprecedented 2015/16 Tasman Sea marine heatwave.. 2017. https://doi.org/10.1038/ncomms16101

Paper 0 details how ocean currents and heat convergence drive anomalous warming patterns in the Tasman Sea.

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More for · 2
Recorded source metadata

Christopher Y. S. Bull, Andrew E. Kiss, Nicolas C. Jourdain, Matthew H. England, Erik van Sebille. Wind Forced Variability in Eddy Formation, Eddy Shedding, and the Separation of the East Australian Current. 2017. https://doi.org/10.1002/2017jc013311

Paper 1 demonstrates how wind stress variability and currents produce complex eddy formation and circulation patterns in the Tasman Sea.

Recorded source metadata

Shears NT, Bowen MM. Half a century of coastal temperature records reveal complex warming trends in western boundary currents.. 2017. https://doi.org/10.1038/s41598-017-14944-2

Paper 4 highlights spatial and temporal complexity in boundary current warming patterns resulting from regional-scale circulation and wind stress.

The paper trail · every fact has a biography
first checked02 Aug 2026
judged → SUPPORTED · 8802 Aug 2026
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