“…Unfortunately, the consequences of such events are difficult to predict by SDMs because extremes and local variability are poorly resolved in projected scenarios of ocean warming. Furthermore, indirect effects associated with changing consumer pressure, for example, due to current‐driven range‐shifting tropical herbivores (Nakamura, Feary, Kanda, & Yamaoka, ; Wernberg, Bennett et al., ), are unaccounted for in climate projections but could accelerate the retreat of temperate seaweeds (Vergés et al., , ; Zarco‐Perello, Wernberg, Langlois, & Vanderklift, ). Thus, thermal anomalies driven by variation in mesoscale warm currents, episodic heatwaves and cascading biological responses add a layer of concern above the predicted declines based on forecasted increases in baseline temperatures (this study, but also see Molinos et al., ).…”