ORIGINAL PAPER
Computational environment HYDRO-PATH as a flexible tool for the operational rainfall-runoff model design
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2Wrocław University of Environmental and Life Sciences, The faculty of Environmental Engineering and Geodesy
3
Wrocław University of Technology Institute of Computer Engineering, Control and Robotics
Publication date: 2016-06-23
Meteorology Hydrology and Water Management, 4(1),65-77
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ABSTRACT
The overall objective of the ongoing work is to develop the computational environment HY DRO-PATH as
a flexible tool for forecasting runoff from catchment areas for various hydrometeorological conditions while taking
into account the information available on a real-time basis. Ensuring the model’s operational reliability and reducing
the uncertainty of generated forecasts is accomplished through the adjustment of both the internal structure of the
model and the spatial representation of the computational grid to the physiographical, hydrological and climatological
characteristics of a given basin. The research focused on the development of methods for selecting the optimal model
structure and parameters by analysing the results obtained for different model structures. This is achieved through the
computational environment, in which it is possible to implement different types of hydrological rainfall-runoff models.
These models have a unified system of data input, parameter optimisation rules, and procedures for result generation.
The developed elements of the computational environment correspond to generation potential of models with
a given structure and complexity. Furthermore, within the framework of HY DRO-PATH the following components
were developed: an application programming interface (API), a data assimilation module, a module for computational
representation of a real object, and a module for the estimation and optimisation of model parameters. The developed
computational environment was applied to prepare a version of TOPO-Flex and perform hydrological validation of
the model’s results. The hydrological validation was performed for selected flood events in the Bystrzyca Dusznicka
subbasin of the Nysa Kłodzka River.