Simulated tropical stratospheric upwelling and O$_{3}$ interactions with the 1D RCE model konrad

Model output of the control and CO$_{2}$-doubling experiments with the 1D radiative-convective equilibrium (RCE) model `konrad`. The model output consists of temperature, atmospheric composition, radiative flux, heating rate profiles, time series of the convective top, surface temperature, and the net radiative flux at the top of the atmosphere. It also includes metadata such as the parameters used for each run.

The experiments varied the relative humidity profile, the representation of O$_{3}$ chemistry, and, more importantly, a parameterization of the cooling due to the tropical stratospheric upwelling caused by the Brewer-Dobson Circulation. With the dataset, one can study the effects the tropical stratospheric upwelling on the tropical equilibrium climate sensitivity.