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. 2020 Jun 3;6(23):eaaz5006. doi: 10.1126/sciadv.aaz5006

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Copyright © 2020 The Authors, some rights reserved; exclusive licensee American Association for the Advancement of Science. No claim to original U.S. Government Works. Distributed under a Creative Commons Attribution License 4.0 (CC BY).

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Fig. 6 — Zonal mean atmospheric temperature (°C) (A to D) and zonal wind (m/s) (F to I) anomalies over the equatorial Pacific region (120°E to 90°W) in the summer (June to September) following the TrNH (A, B, F, and G) and TrSH (C, D, H, and I) eruptions for each ensemble. Bottom panels show the difference between El Niño and La Niña composite for temperature (E) and zonal wind (J). Only values that are significantly different at the 5% level using a local (grid-point) t test are shaded. The contours follow the color bar intervals (solid for positive and dashed for negative anomalies; the zero line is omitted).