Katja Lorbacher

TL;DR: The MAGICC sea level model as discussed by the authors provides a flexible and efficient platform for the analysis of major scenario, model, and climate uncertainties underlying long-term SLR projections, which can be used as a tool to directly investigate the SLR implications of different mitigation pathways and may also serve as input for regional SLR assessments via component-wise sea level pattern scaling.

TL;DR: This paper showed that Southern Hemisphere subtropical drying is not a feature of warm climates per se, but is primarily a response to rapidly rising forcing and global temperatures, as tropical sea surface temperatures rise more than southern subtropically sea-surface temperatures under transient warming, which may represent very different conditions from both past and future "equilibrium" warmer climates.