Fig. 6: Schematic diagram of distinct impacts of the two types of Atlantic Niño on West Antarctic sea ice.
From: Distinct Impacts of the Central and Eastern Atlantic Niño on West Antarctic Sea Ice
a The CAN influences the West Antarctic sea ice through two atmospheric Rossby wave trains, both directly and indirectly. b The EAN can only impact the West Antarctic sea ice indirectly by inducing an atmospheric wave train.
