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Geo-morphological analysis of a watershed is usually used for evolving the regional hydrological models for resolving different hydrological difficulties of the ungauged watersheds in the absence of data accessibility conditions (Gajbhiye et al. 2014).
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Many digital elevation models (DEMs) have difficulty replicating hydrological patterns in flat landscapes.
Regionalization procedures are an important tool for estimating streamflow hydrography; however, there are difficulties associated with properly evaluating hydrological processes.
Various researchers attempting to model hydrological processes at the scale of drainage basin have found difficulties extracting, synthesizing and aggregating data from limited number of locations (Stuart and Stocks 1993; Singh et al. 2013) and finding the suitable data for fully distributed models such as Institute of Hydrology Distributed Model (IHDM) or the Systeme Hydrologique European (SHE).
To overcome this difficulty, we proposed a double-layer parallel system for hydrological model calibration using high-performance computing (HPC) systems.
The feasibility and potential difficulties of the proposed approach are demonstrated by the application to a simple hydrological model.
Uncertainties and inconsistencies in LULC maps are one of the difficulties that LULC timeseries analysis face and which have a significant effect on hydrological impact analysis.
Hydrological Sci.
Hydrological Res.
D.H.S. performed GIS and hydrological analyses.
Loon, A. F. V. Hydrological drought explained.
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