“…For the distant zones T31 (5.24-28.8km) ad T32 (28.8-166.7km) we used the SRTM (Jarvis et al, 2008) with resolution 3 and 30 arcsec, respectively. For the nearer zones T1 (0-250 m) and T2 (250-5240 m) we use standardly the above mentioned detailed model DMR-3 (TOPÚ, 2012), while in the innermost zone we use the concept of interpolated heights, which reduces the computation error originating from the misalignment of DTM with the real height of measured points (Zahorec, 2015). However, for the most accurate computations even this model becomes insufficient.…”