Non super-Clausius-Clapeyron scaling of convective precipitation extremes

This dataset contains data underlying Figure 2, 3, and 4 of the article "Super-Clausius-Clapeyron scaling of extreme precipitation explained by shift from stratiform to convective rain type". Specifically, it contains the scalings of total, convective, and stratiform precipitation extremes with dew point temperature conditioned on all events and conditioned on Mesoscale Convective Systems event (Fig.2), the scalings of precipitation extremes conditioned on the distance to the nearest lightning strike and the associated mean slopes over the dew point temperature range (Fig. 3), Intensity-Duration-Frequency curves for the 5 years return period and conditioned on dew-point temperatures (Fig. 4).