Fig. 5: Seasonal cycles of TBC, \({\mathrm{EP}}_{\ell }^{{\mathrm{Cg}}}\) and EKE in the upper 200 m in eddy-rich simulations. | Nature Climate Change

Fig. 5: Seasonal cycles of TBC, \({\mathrm{EP}}_{\ell }^{{\mathrm{Cg}}}\) and EKE in the upper 200 m in eddy-rich simulations.

From: Eddy activity in the Arctic Ocean projected to surge in a warming world

Fig. 5: Seasonal cycles of TBC, $${\mathrm{EP}}_{\ell }^{{\mathrm{Cg}}}$$ EP ℓ Cg and EKE in the upper 200 m in eddy-rich simulations.

a–c, The difference of TBC integrated over upper 200 m (pink) and the surface power \({\mathrm{EP}}_{\ell }^{{\mathrm{Cg}}}\) at ℓ = 50 km (blue) between the period 2092–2095 and the period 2012–2015 for the Arctic Ocean (a), the Eurasian Basin (b) and the Canada Basin (c). d–f, The difference of EKE over upper 200 m between the two periods for the Arctic Ocean (d), the Eurasian Basin (e) and the Canada Basin (f).

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