“…Near the poleward limits of mangroves in North America, declines in the occurrence of extreme winter temperature events have been identified as a primary driver of mangrove survival and expansion in recent decades (Cavanaugh et al., ; Stevens, Fox, & Montague, ). Biotic interactions between mangrove and marsh species, plus positive biological feedbacks (such as increased resilience to frost damage with mangrove age), may also influence the distribution and rate of mangrove expansion and salt marsh loss, beyond what would be predicted from temperature changes alone (Guo, Zhang, Lan, & Pennings, ; Howard et al., ; Osland et al., ; Peterson & Bell, ). The drivers of within‐range mangrove expansion are less clear and may include rises in relative sea level (whereby mangroves migrate upslope into salt marshes) (Kelleway et al., ; Raabe, Roy, & McIvor, ; Rogers, Battley, et al., , Rogers, Wilton, & Saintilan, ); changing rainfall patterns (Eslami‐Andargoli, Dale, Sipe, & Chaseling, ); increasing atmospheric CO 2 concentration and soil nutrients (McKee, Rogers, & Saintilan, ; McKee & Rooth, ); sedimentation and geomorphic change associated with catchment land use (Swales et al., ); changes in tidal influence and freshwater inflow (Howard et al., ), among other factors (Saintilan & Williams, ).…”