From literature five methods for the detection of summer hail using Radar reflectivity have been selected. First of all, the method based on the bare Radar reflectivity with a threshold and that on the Vertically Integrated Liquid (VIL) with a threshold are selected. The method developed recently in New Zealand by Auer, in which Radar reflectivity is combined with cloud-top temperatures, is selected as well. Finally, the two methods which are currently in use within the framework of NEXRAD, i.e., the method of Waldvogel and the Severe Hail Index (SHI), are chosen. These five different methods have been tested on severe weather events in the Netherlands during the summer of 1999. As ground truth, observations by the 321 volunteers of the (rainfall) observer network of the KNMI as well as detailed hail damage reports from agricultural insurance companies have been taken. Evidently, some hail events will not have been observed due to their small spatial extent and/or their short time duration. Both the effect of this incomplete ground truth dataset as the effect of possible spatial mismatches between the high-altitude Radar observations and the ground truth observations on the scoring parameters, like the Critical Success Index (CSI), have been investigated. The results of the comparison between these five methods for detection of hail will be presented in detail.