The global overturning circulation is the way the ocean exchanges water around the globe, with sinking of cold, dense water in the North Atlantic and Southern Ocean, and upwelling in the Southern Ocean. This moves heat, nuturients, and gasses around the globe and impacts climate on decadal to millenial time scales. In our group we study the physics of this overturning circulation by identifiying tipping points in the circulation and simplifying the physics to simple scaling laws.