A pole-to-equator ocean overturning circulation on Enceladus

@article{Lobo2021APO,
  title={A pole-to-equator ocean overturning circulation on Enceladus},
  author={Ana H. Lobo and Andrew F. Thompson and Steven Douglas Vance and Saikiran Tharimena},
  journal={Nature Geoscience},
  year={2021},
  volume={14},
  pages={185 - 189}
}
Enceladus is believed to have a saltwater global ocean, heated at the ocean–core interface and losing heat to the floating ice shell above. This configuration suggests an important role for vertical convection. The ice shell has dramatic meridional thickness variations that, in steady state, must be sustained by the ocean circulation against processes acting to remove these anomalies. This could be achieved through spatially separated regions of freezing and melting at the ocean–ice interface… 
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