Ognjen Bonacci

Prof. Dr. Ognjen Bonacci

Architecture and Geodesy, Faculty of Civil Engineering, Split University, Poljička cesta 35, 21000 Split, Croatia
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Research Focus & Metrics

Academic Career Length

48Years (1979-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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11 August 2017 in Science
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Günter BlöschlGünter Blöschl
Günter Blöschl
JHJulia Hall
Julia Hall
Juraj ParajkaJuraj Parajka
Juraj Parajka
Rui A. P. PerdigãoRui A. P. Perdigão
Rui A. P. Perdigão
BMBruno Merz
Bruno Merz
NŽNenad Živković
Nenad Živković
Flooding along the river: Will a warming climate affect river floods? The prevailing sentiment is yes, but a consistent signal in flood magnitudes has not been found. Blöschl et al. analyzed the timing of river floods in Europe over the past 50 years and found clear patterns of changes in flood timing that can be ascribed to climate effects (see the Perspective by Slater and Wilby). These variations include earlier spring snowmelt floods in northeastern Europe, later winter floods around the North Sea and parts of the Mediterranean coast owing to delayed winter storms, and earlier winter floods in western Europe caused by earlier soil moisture maxima. Science , this issue p. 588 see also p. 552

1 February 1993 in Hydrological Sciences Journal
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Ognjen BonacciOgnjen Bonacci
Ognjen Bonacci
By analysing the hydrographs of karst springs it is possible to identify aquifer characteristics and, accordingly, the main features of a karst rock-fissure massif. Consequently, relevant data can be obtained by analysing hydrograph recession curves. This paper presents a detailed analysis and explanation of numerous cases of break points on recession curves via various values of the recession coefficient α in Maillet's (1905) equation. The paper also identifies the relationship between α and a linear reservoir coefficient by employing groundwater hydrograph methods. It is shown that the linear reservoir coefficient changes with time in accordance with changes of the flow conditions in the karst massif.

23 January 2008 in Environmental Geology
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Ognjen BonacciOgnjen Bonacci
Ognjen Bonacci
Tanja PipanTanja Pipan
Tanja Pipan
DCDavid C. Culver
David C. Culver

31 March 2006 in Natural Hazards and Earth System Sciences
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Ognjen BonacciOgnjen Bonacci
Ognjen Bonacci
ILI. Ljubenkov
I. Ljubenkov
TRT. Roje-Bonacci
T. Roje-Bonacci
Flash floods constitute one of the deadliest and costliest natural disasters worldwide. This paper explains the karst flash flood phenomenon, which represents a special kind of flash flood. As the majority of flash floods karst flash floods are caused by intensive short-term precipitation in an area whose surface rarely exceeds a few square kilometres. The characteristics of all flash floods are their short duration, small areal extent, high flood peaks and rapid flows, and heavy loss of life and property. Karst flash floods have specific characteristics due to special conditions for water circulation, which exist in karst terrains. During karst flash floods a sudden rise of groundwater levels occurs, which causes the appearance of numerous, unexpected, abundant and temporary karst springs. This paper presents in detail an example of a karst flash flood in the Marina bay (Dinaric karst region of Croatia), which occurred in December 2004.

30 April 2019 in Water Resources Management
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BHBahrudin Hrnjica
Bahrudin Hrnjica
Ognjen BonacciOgnjen Bonacci
Ognjen Bonacci

22 September 2006 in Hydrological Processes
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CPCvetanka Popovska
Cvetanka Popovska
Ognjen BonacciOgnjen Bonacci
Ognjen Bonacci