Fig. 5: Community earth system model experiments.
From: Distinct Impacts of the Central and Eastern Atlantic Niño on West Antarctic Sea Ice
a Differences of JJA 200-hPa GPH (shading, m) and WAF (vector, m2 s−2) between the central Atlantic Niño (CAN) experiment and the control run (CTRL). b Same as (a) but for the eastern Atlantic Niño (EAN) experiment. Black contours denote GPH anomalies that are statistically significant at 90% confidence level. The magenta (green) line represents the wave train propagation pathway generated by the direct (indirect) impact of Atlantic Niño on Antarctica. c Differences of JJA precipitation (shading, mm day−1) and 200-hPa divergent wind (vector, m s−1) between the CAN experiment and the CTRL. d Same as (c) but for the EAN experiment. Stippling and black vectors represent anomalies that are statistically significant at the 90% confidence level.
