Titlebook: Surface Models for Geosciences; Kateřina Růžičková,Tomáš Inspektor Book 2015 Springer International Publishing Switzerland 2015 Analysis O

凝结剂

极肥胖

Results Comparison of the Flow Direction and Accumulation Algorithms Together with Distributed Rainlatforms ESRI ArcGIS and IDRISI used in this case study and also the used open source tools such as GRASS GIS or SAGA GIS dispose of such modules. It is expected that the currently established algorithms generate good enough results, so crucial factors for such analyses become quality and resolution

宽宏大量

连锁

弯弯曲曲

DTM Impact on the Results of Dam Break Simulation in 1D Hydraulic Models, software packages USACE HEC-RAS and DHI MIKE 11 worldwide including the Czech Republic. Coincidentally, at this level, both previously mentioned hydraulic models are using identical numerical solvers DAMBRK and WSPRO. It can be expected that the use of identical schematization of the river channels

Interim

reception

Geographic Information System for Flood Hazard Analysis and Early Warning Using Numerical Weather Pre of a flooding has been well researched, and several methods of flood hazard simulation have been established over the last decades. The current legislation in the European Union requires the Member States to create, maintain and update flood risk and hazard maps, as well as identify possible sour

娴熟

helper-T-cells

Creating of DSM Based on RPAS Measurement and Accuracy Testing,in 2011. The project’s aim was to develop, test and verify simple and low-cost technology for the monitoring and modelling of small areas such as archaeological digs, historical objects, dumps, mines or and small orthophoto projects. The creation of a digital surface model from photos and its accura

协迫

The Use of Real and Fictitious Surfaces for Territorial Distribution Assessment of Given Geographica major distribution factor of processes in the landscape. This concept is related to both continuous (e.g. air temperature, rainfall) and a discrete (various forms of land use) phenomena. While at continuous phenomena simulated surfaces of terrain distributed phenomena respect the configuration of