Intensified atmospheric branch of the hydrological cycle over the Tibetan Plateau during the Last Interglacial from a dynamical downscaling perspective

<p>We provide the datasets run for&nbsp;investigating&nbsp;the atmospheric branch of the hydrological cycle over the Tibetan Plateau during the Last Interglacial (127 ka), based on the &nbsp;mesoscale Weather Research and Forecasting (WRF) model driven by the Community Earth System Model (CESM). We upload summer mean of the model outputs&nbsp;from the WRF over the Tibetan Plateau used in estimating the atmospheric branch of the hydrological cycle.</p>