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Günter Blöschl

Researcher at Vienna University of Technology

Publications -  430
Citations -  35204

Günter Blöschl is an academic researcher from Vienna University of Technology. The author has contributed to research in topics: Flood myth & Surface runoff. The author has an hindex of 90, co-authored 387 publications receiving 29536 citations. Previous affiliations of Günter Blöschl include Australian National University & University of Vienna.

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Scale issues in hydrological modelling: A review

TL;DR: A framework is provided for scaling and scale issues in hydrology and a more holistic perspective dealing with dimensional analysis and similarity concepts is addressed, which deals with complex processes in a much simpler fashion.
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A decade of Predictions in Ungauged Basins (PUB)—a review

TL;DR: The Prediction in Ungauged Basins (PUB) initiative of the International Association of Hydrological Sciences (IAHS) launched in 2003 and concluded by the PUB Symposium 2012 held in Delft (23-25 October 2012), set out to shift the scientific culture of hydrology towards improved scientific understanding of hydrological processes, as well as associated uncertainties and the development of models with increasing realism and predictive power as discussed by the authors.
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Socio‐hydrology: A new science of people and water

TL;DR: Murugesu Sivapalan,* Hubert H. G. Savenije and Gunter Bloschl 1 Department of Civil and Environmental Engineering, Department of Geography, University of Illinois at Urbana-Champaign, UrbANA, IL 61801, USA as mentioned in this paper.
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Observed spatial organization of soil moisture and its relation to terrain indices

TL;DR: In this paper, the authors analyzed the degree of spatial organization of soil moisture and the ability of terrain attributes to predict that organization using point measurements from the 10.5 ha Tarrawarra experimental catchment in Australia.
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Preferred states in spatial soil moisture patterns: Local and nonlocal controls

TL;DR: In this paper, the authors developed a conceptual and observational case in which soil water patterns in temperate regions of Australia switch between two preferred states: the wet state is dominated by lateral water movement through both surface and subsurface paths, with catchment terrain leading to organization of wet areas along drainage lines.