Extended Data Fig. 7: Climate responses in the Indian Ocean for different patterns of cooling in the North Atlantic.
From: Tropical response to ocean circulation slowdown raises future drought risk
Changes in annual-mean rainfall (a–d) and surface air temperature (e–h) averaged across simulations with different combinations of strong and muted cooling in the high latitude and tropical North Atlantic. The simulations in each group are listed below each panels title. The values of strong and weak high latitude cooling range from −20 to −8 K and from −7 to −1 K respectively. The values of strong/moderate and weak tropical cooling range from −5.5 to −1 K and from −1 to 0 K respectively.
