Pierluigi Claps

Dr. Pierluigi Claps

Politecnico di Torino, Turin, Piedmont, Italy
orcid

Research Focus & Metrics

Academic Career Length

35Years (1992-Present)

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

Representative Publications

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28 August 2019 in Nature
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Journal Article
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Günter BlöschlGünter Blöschl
Günter Blöschl
JHJulia Hall
Julia Hall
AVAlberto Viglione
Alberto Viglione
Rui A. P. PerdigãoRui A. P. Perdigão
Rui A. P. Perdigão
JPJuraj Parajka
Juraj Parajka
NŽNenad Živković
Nenad Živković

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

2 July 2019 in Hydrological Sciences Journal
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Journal Article
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Günter BlöschlGünter Blöschl
Günter Blöschl
MBMarc F.P. Bierkens
Marc F.P. Bierkens
ACAntonio Chambel
Antonio Chambel
CCChristophe Cudennec
Christophe Cudennec
Georgia  DestouniGeorgia Destouni
Georgia Destouni
Yongqiang ZhangYongqiang Zhang
Yongqiang Zhang
This paper is the outcome of a community initiative to identify major unsolved scientific problems in hydrology motivated by a need for stronger harmonisation of research efforts. The procedure involved a public consultation through on-line media, followed by two workshops through which a large number of potential science questions were collated, prioritised, and synthesised. In spite of the diversity of the participants (230 scientists in total), the process revealed much about community priorities and the state of our science: a preference for continuity in research questions rather than radical departures or redirections from past and current work. Questions remain focussed on process-based understanding of hydrological variability and causality at all space and time scales. Increased attention to environmental change drives a new emphasis on understanding how change propagates across interfaces within the hydrological system and across disciplinary boundaries. In particular, the expansion of the human footprint raises a new set of questions related to human interactions with nature and water cycle feedbacks in the context of complex water management problems. We hope that this reflection and synthesis of the 23 unsolved problems in hydrology will help guide research efforts for some years to come.

30 July 2014 in Hydrology and Earth System Sciences
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JHJulia Hall
Julia Hall
BABerit Arheimer
Berit Arheimer
MBMarco Borga
Marco Borga
RBR. Brázdil
R. Brázdil
PCPierluigi Claps
Pierluigi Claps
Günter BlöschlGünter Blöschl
Günter Blöschl
There is growing concern that flooding is becoming more frequent and severe in Europe. A better understanding of flood regime changes and their drivers is therefore needed. The paper reviews the current knowledge on flood regime changes in European rivers that has traditionally been obtained through two alternative research approaches. The first approach is the data-based detection of changes in observed flood events. Current methods are reviewed together with their challenges and opportunities. For example, observation biases, the merging of different data sources and accounting for nonlinear drivers and responses. The second approach consists of modelled scenarios of future floods. Challenges and opportunities associated with flood change scenarios are discussed such as fully accounting for uncertainties in the modelling cascade and feedbacks. To make progress in flood change research, we suggest that a synthesis of these two approaches is needed. This can be achieved by focusing on long duration records and flood-rich and flood-poor periods rather than on short duration flood trends only, by formally attributing causes of observed flood changes, by validating scenarios against observed flood regime dynamics, and by developing low-dimensional models of flood changes and feedbacks. The paper finishes with a call for a joint European flood change research network.

1 November 2010 in Journal of Hydrology
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Journal Article
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Juraj ParajkaJuraj Parajka
Juraj Parajka
SKS. Kohnová
S. Kohnová
GBG. Bálint
G. Bálint
MBM. Barbuc
M. Barbuc
MBMarco Borga
Marco Borga
Günter BlöschlGünter Blöschl
Günter Blöschl
The aim of this paper is to analyse the differences in the long-term regimes of extreme precipitation and floods across the Alpine–Carpathian range using seasonality indices and atmospheric circulation patterns to understand the main flood-producing processes. This is supported by cluster analyses to identify areas of similar flood processes, both in terms of precipitation forcing and catchment processes. The results allow to isolate regions of similar flood generation processes including southerly versus westerly circulation patterns, effects of soil moisture seasonality due to evaporation and effects of soil moisture seasonality due to snow melt. In many regions of the Alpine–Carpathian range, there is a distinct shift in flood generating processes with flood magnitude as evidenced by a shift from summer to autumn floods. It is argued that the synoptic approach proposed here is valuable in both flood analysis and flood estimation.

20 March 2007 in Water Resources Research
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Journal Article
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AVA. Viglione
A. Viglione
FLF. Laio
F. Laio
PCPierluigi Claps
Pierluigi Claps