Alessandro Corsini

Dr. Alessandro Corsini

University of Modena and Reggio Emilia, Department of Chemical and Geological Sciences, Modena, Italy
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Research Focus & Metrics

Academic Career Length

23Years (2004-Present)

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

Representative Publications

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27 October 2005 in Landslides
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TSTazio Strozzi
Tazio Strozzi
PFPaolo Farina
Paolo Farina
ACAlessandro Corsini
Alessandro Corsini
CAChristian Ambrosi
Christian Ambrosi
MTManfred Thüring
Manfred Thüring
CWCharles Werner
Charles Werner

1 January 2004 in CATENA
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Journal Article
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Mauro SoldatiMauro Soldati
Mauro Soldati
ACAlessandro Corsini
Alessandro Corsini
APAlessandro Pasuto
Alessandro Pasuto


10 April 2010 in Landslides
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FEDERICO CERVIFEDERICO CERVI
FEDERICO CERVI
MBMatteo Berti
Matteo Berti
Lisa BorgattiLisa Borgatti
Lisa Borgatti
Francesco RonchettiFrancesco Ronchetti
Francesco Ronchetti
FMFederica Manenti
Federica Manenti
ACAlessandro Corsini
Alessandro Corsini

1 January 2013 in Geomorphology
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Journal Article
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MBMatteo Berti
Matteo Berti
ACAlessandro Corsini
Alessandro Corsini
ADAlexander Daehne
Alexander Daehne

6 August 2013 in Natural Hazards and Earth System Sciences
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Journal Article
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Matteo BertiMatteo Berti
Matteo Berti
ACAlessandro Corsini
Alessandro Corsini
SFS. Franceschini
S. Franceschini
JIJ. P. Iannacone
J. P. Iannacone
We present a new method for the automatic classification of Persistent Scatters Interferometry (PSI) time series based on a conditional sequence of statistical tests. Time series are classified into distinctive predefined target trends, such as uncorrelated, linear, quadratic, bilinear and discontinuous, that describe different styles of ground deformation. Our automatic analysis overcomes limits related to the visual classification of PSI time series, which cannot be carried out systematically for large datasets. The method has been tested with reference to landslides using PSI datasets covering the northern Apennines of Italy. The clear distinction between the relative frequency of uncorrelated, linear and non-linear time series with respect to mean velocity distribution suggests that different target trends are related to different physical processes that are likely to control slope movements. The spatial distribution of classified time series is also consistent with respect the known distribution of flat areas, slopes and landslides in the tests area. Classified time series enhances the radar interpretation of slope movements at the site scale, pointing out significant advantages in comparison with the conventional analysis based solely on the mean velocity. The test application also warns against potentially misleading classification outputs in case of datasets affected by systematic errors. Although the method was developed and tested to investigate landslides, it should be also useful for the analysis of other ground deformation processes such as subsidence, swelling/shrinkage of soils, or uplifts due to deep injections in reservoirs.