Abstract Paleoclimate records have been used to estimate the modern equilibrium climate sensitivity. However. this requires understanding how the feedbacks governing the climate response vary with the climate itself. Here we warm and cool a state-of-the-art climate model to simulate a continuum of climates ranging from a nearly ice-covered Snowball Earth to a nearly ice-free hothouse. https://www.greenresourcesredux.com/product-category/rasiercreme/