Sybren Drijfhout

Shutdown of northern Atlantic overturning after 2100 following deep mixing collapse in CMIP6 projections

Ocean Heat Convergence and North Atlantic Multidecadal Heat Content Variability

Communicating future sea-level rise uncertainty and ambiguity to assessment users

The decrease in ocean heat transport in response to global warming

Antarctic contribution to future sea level from ice shelf basal melt as constrained by ice discharge observations

Circulation adjustment in the Arctic and Atlantic in response to Greenland and Antarctic mass loss

The Atlantic Meridional Overturning Circulation in High‐Resolution Models

Sensitivity of the Atlantic Meridional Overturning Circulation to Model Resolution in CMIP6 HighResMIP Simulations and Implications for Future Changes

Precession‐ and Obliquity‐Induced Changes in Moisture Sources for Enhanced Precipitation Over the Mediterranean Sea

Ocean and atmosphere influence on the 2015 European heatwave

Atlantic-Pacific Asymmetry in Deep Water Formation

Response of the Asian summer monsoons to idealized precession and obliquity forcing in a set of GCMs

Sinking of Dense North Atlantic Waters in a Global Ocean Model: Location and Controls

Lagrangian ocean analysis: Fundamentals and practices

A high-end sea level rise probabilistic projection including rapid Antarctic ice sheet mass loss

Resolution dependence of extreme precipitation and deep convection over the <scp>G</scp>ulf <scp>S</scp>tream

Precession and obliquity forcing of the freshwater budget over the Mediterranean

Response of the North African summer monsoon to precession and obliquity forcings in the EC-Earth GCM

Historical and idealized climate model experiments: an intercomparison of Earth system models of intermediate complexity

Spontaneous abrupt climate change due to an atmospheric blocking–sea-ice–ocean feedback in an unforced climate model simulation

Conceptual Models of the Wind-Driven and Thermohaline Circulation

Monsoonal response to mid-holocene orbital forcing in a high resolution GCM

Sensitivity of the Atlantic meridional overturning circulation to South Atlantic freshwater anomalies