Stronger vertical mixing invigorates the MOC [Meridonal Overturning Circulation] by an order of magnitude, increases
ocean heat transport by 50 — 100 %, reduces the zonal mean equator - to - pole temperature gradients by up to 6 °C, lowers tropical
peak terrestrial temperatures by up to 6 °C, and warms high - latitude
oceans by up to 10 °C.»