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