Fluvi�ln� procesy
Znamen� to, �e geosyst�my se sna�� dos�hnout stavu rovnov�hy, kter� se projevuje bu� st�lost� struktury syst�mu (nap�. stejn�m po�tem p��tok� vodn�ho toku), nebo
Znamen� to, �e geosyst�my se sna�� dos�hnout stavu rovnov�hy, kter� se projevuje bu� st�lost� struktury syst�mu (nap�. stejn�m po�tem p��tok� vodn�ho toku), nebo
Marek Haluska Ing. Daniel Novický Ing. Pavel Kodytek Ing. Roman Kulštejn Ing. Bára Janošcová Bc. Václav Hanke Bc. Jan Ručka Ing. Lukáš Danys, Ph.D. Ing. Šárka Vávrová
Marek Haluska Ing. Daniel Novický Ing. Pavel Kodytek Ing. Roman Kulštejn Ing. Bára Janošcová Bc. Václav Hanke Bc. Jan Ručka Ing. Lukáš Danys, Ph.D. Ing. Šárka Vávrová
David Barabasz Ing. Alexandra Bodzás Ing. Pavel Kodytek Ing. Bára Janošcová Bc. Václav Hanke Ing. Rostislav Pokorný Ing. Vít Jandásek Ing. Tomáš Skotnica Bc. Martin
Martin Mikulášek Ing. Martin Kryl Ing. Alexandra Bodzás Ing. Pavel Kodytek Ing. Bára Janošcová Bc. Lukáš Krais Ing. Jan Jašek Bc. Dominik Pieter Ing. Jakub Štefanský
REKA: Amsterdam University of Applied Sciences Edinburgh Napier University Frankfurt University of Applied Sciences HOGENT University of Applied Sciences and Arts Metropolia University of Applied
Marek Haluska Ing. Daniel Novický Ing. Pavel Kodytek Ing. Roman Kulštejn Ing. Bára Janošcová Bc. Václav Hanke Bc. Jan Ručka Ing. Lukáš Danys, Ph.D. Ing. Šárka Vávrová
David Barabasz Ing. Alexandra Bodzás Ing. Pavel Kodytek Ing. Bára Janošcová Bc. Václav Hanke Ing. Rostislav Pokorný Ing. Vít Jandásek Ing. Tomáš Skotnica Bc. Martin
This makes extra difficulties for the DEM generation. We focused on extraction of terrain (bare earth) points from point cloud using a number of different filtering
Martin Mikulášek Ing. Martin Kryl Ing. Alexandra Bodzás Ing. Pavel Kodytek Ing. Bára Janošcová Bc. Lukáš Krais Ing. Jan Jašek Bc. Dominik Pieter Ing. Jakub Štefanský