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Assessing the added value of the Intermediate Complexity Atmospheric Research (ICAR) model for precipitation in complex topography

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Figure

Figure 1. The South Island of New Zealand. Shown are the coast(black line), the topography above an elevation of 1000mm.s.l.(gray shading), glacierized areas (blue shading), the approximatelocation of the main alpine crest (red line) and the location of te
Table 1. List of weather stations used in this study sorted by their elevation. The table lists the station number (No.), elevation ((Lat), longitude (Long), name, average distance downwind of the main crest of the Southern Alps (University of Otago (3)
Figure 2. The average (a) and MSE (b) SSMSE of ICAR and ICARCP time series from simulations for the reference period from 2014 to2015 at alpine weather stations as a function of the chosen model top (in kilometers above topography)
Table 2. Time series characteristics for all of the weather stations, as well as a detailed overview of performance metrics for both ICARCPand ERAI obtained for each individual site
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