• Non ci sono risultati.

Investigation on rainfall extremes events trough a geoadditive model

N/A
N/A
Protected

Academic year: 2021

Condividi "Investigation on rainfall extremes events trough a geoadditive model"

Copied!
1
0
0

Testo completo

(1)

Geophysical Research Abstracts Vol. 14, EGU2012-11665-1, 2012 EGU General Assembly 2012 © Author(s) 2012

Investigation on rainfall extremes events trough a geoadditive model

C. Bocci (1), E. Caporali (2), A. Petrucci (3), and G. Rossi (2)

(1) IRPET · Istituto Regionale per la Programmazione Economica della Toscana, (2) University of Firenze, Department of Civil and Environmental Engineering, (3) University of Firenze, Department of Statistics “G. Parenti”

Rainfall can be considered a very important variable, and rainfall extreme events analysis of great concern for the enormous impacts that they may have on everyday life particularly when related to intense rainfalls and floods, and hydraulic risk management. On the catchment area of Arno River in Tuscany, Central Italy, a geoadditive mixed model of rainfall extremes is developed. Most of the territory of Arno River has suffered in the past of many severe hydro-geological events, with high levels of risk due to the vulnerability of a unique artistic and cultural heritage. The area has a complex topography that greatly influences the precipitation regime. The dataset is composed by the time series of the annual maxima of daily rainfall recorded in about 400 rain gauges, spatially distributed over the catchment area of about 8.800 km2. The record period covers mainly the second half of 20th century. The rainfall observations are assumed to follow generalized extreme value distributions whose locations are spatially dependent and where the dependence is captured using a geoadditive model. In particular, since rainfall has a natural spatial domain and a significant spatial variability, a spatial hierarchical model for extremes is used. The spatial hierarchical models, in fact, take into account data from all locations, borrowing strength from neighbouring locations when they estimate parameters and are of great interest when small set of data is available, as in the case of rainfall extreme values. Together with rain gauges location variables further physiographic variables are investigated as explanation variables. The implemented geoadditive mixed model of spatially referenced time series of rainfall extreme values, is able to capture the spatial dynamics of the rainfall extreme phenomenon. Since the model shows evidence of a spatial trend in the rainfall extreme dynamic, the temporal dynamic and the time influence can be also taken into account. The implemented spatial hierarchical model can be used to produce maps of potential risk for extreme rainfall events to be used in the definition of protection measures as well as to design risk mitigation interventions.

Riferimenti

Documenti correlati

[r]

Innanzitutto, in nessuno degli studi prodotti è stata eseguita una valutazione bioptica renale nei pazienti switchati, in grado di dimostrare un maggior danno podocitario e/o una

8 we present the invariant mass distribution of the two charged leptons and the two jets associated with the vector boson decay for MH  200 GeV and for the no- Higgs case.. A

L’analisi dettagliata delle voci rivela infatti che lo spettro delle opere da cui il testo attinge e` amplissimo e copre diversi settori: gli scrittori di numi- smatica come

refractory disease, relapse within 6 months from autologous stem cell transplantation (ASCT), age, pre-transplant chemotherapy, hematopoietic cell transplantation comorbidity

Vista generale del quartiere Fotainhas, metà XX secolo Largo Actor Dias all’inizio del XX secolo. Vista aerea da Vila Nova de Gaia,

Rispetto a questo interesse pubblico, il diritto dell’individuo non può ritenersi sempre e comunque recessivo (al punto tale da imporre sempre e comunque un intervento

7 displays the time needed to reach the observed deuterium + 2H = 0.04 from a given initial ortho-to-para ratio of fraction of DNfrac H2 shown on the top axis versus the time needed