Fig. 3From: Prediction of volcanic ash concentrations in ash clouds from explosive eruptions based on an atmospheric transport model and the Japanese meteorological satellite Himawari-8: a case study for the Kirishima-Shinmoedake eruption on April 4th 2018a–c Total column mass loadings estimated by OVAA (21:30, 22:30, 23:30UTC). d–f The total column mass loadings in the prediction for the \(T_c\)=0.3. The forecast lead time (FT) for d–f are 1, 2 and 3 h, respectively. g–i Same as d–f, but for \(T_c\)=0.6. j–l Same as d–f, but for \(T_c\)=0.9. m–o The ash concentrations predictions in the ash clouds for \(T_c\)=0.6. The ash concentrations are calculated from tracers in an unit volume with 0.04 degrees (longitude) \(\times\) 0.033 degrees (latitude) \(\times\) 500 m (altitude). The initial time for the prediction (FT=0 h) is set to 20:30UTC (i.e., the initial conditions for JMA–ATM are made from the OVAA estimation at 20:30UTC). The color scale for a–l is shown next to c. The color scale for m–o is shown next to o. The black triangles show the location of the Shinmoedake volcanoBack to article page