CLIMATOLOGICAL STUDY OF THE WIND IN PIEDMONT

The object of the following study is to individualize the common anemological features in the Piemonte region. The executed analysis avails itself of a multiannual sample of wind data (from 1990 to 2000) collected by 59 ARPA-Piemonte monitoring network. The wind statistical analyses have followed different phases: - analyses of wind frequency and wind directions and spotting of the anemological basins; - annual and monthly average of wind directions; - annual monthly and hourly average of the wind force with spotting of breezes; - analyses of daily and hourly wind calm; - analyses of the strongest windblasts with records of critical cases; - analyses of the number of days of föhn and types of weather (Borghi-Giuliacci method)

CLIMATOLOGICAL STUDY OF THE WIND IN PIEDMONT

The object of the following study is to individualize the common anemological features in the Piemonte region. The executed analysis avails itself of a multiannual sample of wind data (from 1990 to 2000) collected by 59 ARPA-Piemonte monitoring network. The wind statistical analyses have followed different phases: - analyses of wind frequency and wind directions and spotting of the anemological basins; - annual and monthly average of wind directions; - annual monthly and hourly average of the wind force with spotting of breezes; - analyses of daily and hourly wind calm; - analyses of the strongest windblasts with records of critical cases; - analyses of the number of days of föhn and types of weather (Borghi-Giuliacci method)

CHANGES IN PRECIPITATION EXTREMES IN BRAZIL (PARANÁ RIVER BASIN)

Made available in DSpace on 2018-12-11T17:00:33Z (GMT). No. of bitstreams: 0 Previous issue date: 2016-02-01This research was aimed at addressing aspects related to variation in the amount of precipitation during the period from 1986 to 2011 in the Paraná River Hydrographical Basin, Brazil, for 32 meteorological stations using 11 climate indices created by the ETCCDI (Expert Team, ET, on Climate Change Detection and Indices, ETCCDI). The daily rainfall data were organized in spreadsheets, which were subjected to an intense quality control and an accurate historical research. For each pluviometric index, we have estimated the trends and the statistical significant of the slopes have been calculated. The results confirm that an increase in total precipitation in almost all analyzed stations was registered, and the extreme precipitations were the main contributors to such additions. In fact, the significant increase in total annual rainfall in north-central sector of the basin are related to higher rates of heavy rain, mainly above 95th percentile, as well as to the highest event of rainfall above 10 mm. Instead the northern part of the region, showed declining trends of extreme rainfall, caused mainly by the reduction in the rainfall occurrences over 95th percentile. In order to evaluate the impact that the increasing extreme rainfall may cause in large urban centers, we have investigated the data of two municipalities (Curitiba, PR and Goiânia, GO-Brazil), where the positive trend can cause inconvenience to the population (floods and inundations) suggesting, at least, the need of implementation of more effective urban planning for the future.Programa de Pós-Graduação em Geografia Universidade Estadual Paulista - UNESP Instituto de Geociências e Ciências Exatas, Avenida 24 A, número 1515Dipartimento di Scienze della Terra Università di Torino, Via Valperga Caluso 35Centro di Ricerca sui Rischi Naturali in Ambiente Montano e Collinare (NatRisk), via Leonardo da Vinci 4Programa de Pós-Graduação em Geografia Universidade Estadual Paulista - UNESP Instituto de Geociências e Ciências Exatas, Avenida 24 A, número 151

Daily oceanographic analyses by the Mediterranean basin scale assimilation system

This study presents the upgrade of the Optimal Interpolation scheme used in the basin scale assimilation scheme of the Mediterranean Forecasting System . The modifications include a daily analysis cycle, the assimilation of ARGO float profiles, the implementation of the geostrophic balance in the background error covariance matrix and the initialisation of the analyses. A series of numerical experiments showed that each modification had a positive impact on the accuracy of the analyses: The daily cycle improved the representation of the processes with a relatively high temporal variability, the assimilation of ARGO floats profiles significantly improved the salinity analyses quality, the geostrophically balanced background error covariances improved the accuracy of the surface elevation analyses, and the initialisation removed the barotropic adjustment in the forecast first time steps starting from the analysis

Mediterranean Sea large-scale low-frequency ocean variability and water mass formation rates from 1987 to 2007: A retrospective analysis

We describe a synthesis of the Mediterranean Sea circulation structure and dynamics from a 23-year- long reanalysis of the ocean circulation carried out by Adani et al. (2011). This mesoscale permitting dynamical reconstruction of past ocean variability in the Mediterranean Sea allows the study of the time-mean circulation and its low frequency, decadal, components. It is found that the time-mean circu- lation is composed of boundary and open ocean intensified jets at the border of cyclonic and anticyclonic gyres. The large scale basin circulation is generally characterized in the northern regions by cyclonic gyres and in its southern parts by anticyclonic gyres and eddy-dominated flow fields, with the exception of the Tyrrhenian and the northern Ionian Sea. The time-mean Tyrrhenian Sea circulation is dominated by cyclonic gyres of different intensity and intermittency. The northern Ionian Sea circulation, however, reverses in sign in two ten-year periods, the first in 1987–1996 and the second in 1997–2006, which is here called the Northern Ionian reversal phenomenon. This reversal is provoked by the excursion of the Atlantic-Ionian Stream from the middle to the northern parts of the basin. The decadal variability of other parts of the basin is characterized by changes in strength of the basin scale structures. The water mass formation rates and variability are dominated by event-like periods where the intermediate and deep waters are formed for 2–3 years at higher rates. The largest deep water formation events of the past 23 years occurred separately in the western and eastern Mediterranean basin: the first coincided with the Eastern Mediterranean Transient (Roether et al., 1996) and the second with the western Mediterranean deep water formation event in 2005–2006 (Smith et al., 2008). A new schematic of the basin-scale circu- lation is formulated and commented.Published318-3324A. Oceanografia e climaJCR Journa