Sea-Level climate variability in the Mediterranean Sea

Sea-level variability is characterized by multiple interacting factors described in the Fourth Assessment Report (Bindoff et al., 2007) of the Intergovernmental Panel on Climate Change (IPCC) that act over wide spectra of temporal and spatial scales. In Church et al. (2010) sea-level variability and changes are defined as manifestations of climate variability and change. The European Environmental Agency (EEA) defines sea level as one of most important indicators for monitoring climate change, as it integrates the response of different components of the Earths system and is also affected by anthropogenic contributions (EEA, 2011). The balance between the different sea-level contributions represents an important source of uncertainty, involving stochastic processes that are very difficult to describe and understand in detail, to the point that they are defined as an enigma in Munk (2002). Sea-level rate estimates are affected by all these uncertainties, in particular if we look at possible responses to sea-level contributions to future climate. At the regional scale, lateral fluxes also contribute to sea-level variability, adding complexity to sea-level dynamics. The research strategy adopted in this work to approach such an interesting and challenging topic has been to develop an objective methodology to study sea-level variability at different temporal and spatial scales, applicable in each part of the Mediterranean basin in particular, and in the global ocean in general, using all the best calibrated sources of data (for the Mediterranean): in-situ, remote-sensig and numerical models data. The global objective of this work was to achieve a deep understanding of all of the components of the sea-level signal contributing to sea-level variability, tendency and trend and to quantify them.

Satellite and in situ data integrated analysis to study the upper ocean an coastal environment of the Italian seas

The thesis objectives are to develop new methodologies for study of the space and time variability of Italian upper ocean ecosystem through the combined use of multi-sensors satellite data and in situ observations and to identify the capability and limits of remote sensing observations to monitor the marine state at short and long time scales. Three oceanographic basins have been selected and subjected to different types of analyses. The first region is the Tyrrhenian Sea where a comparative analysis of altimetry and lagrangian measurements was carried out to study the surface circulation. The results allowed to deepen the knowledge of the Tyrrhenian Sea surface dynamics and its variability and to defined the limitations of satellite altimetry measurements to detect small scale marine circulation features. Channel of Sicily study aimed to identify the spatial-temporal variability of phytoplankton biomass and to understand the impact of the upper ocean circulation on the marine ecosystem. An combined analysis of the satellite of long term time series of chlorophyll, Sea Surface Temperature and Sea Level field data was applied. The results allowed to identify the key role of the Atlantic water inflow in modulating the seasonal variability of the phytoplankton biomass in the region. Finally, Italian coastal marine system was studied with the objective to explore the potential capability of Ocean Color data in detecting chlorophyll trend in coastal areas. The most appropriated methodology to detect long term environmental changes was defined through intercomparison of chlorophyll trends detected by in situ and satellite. Then, Italian coastal areas subject to eutrophication problems were identified. This work has demonstrated that satellites data constitute an unique opportunity to define the features and forcing influencing the upper ocean ecosystems dynamics and can be used also to monitor environmental variables capable of influencing phytoplankton productivity.

Sintesi e caratterizzazione di nuovi copoliesteri alifatici multiblocco per applicazioni biomedicali

La ricerca nell’ambito dell’ingegneria tissutale e del rilascio controllato di farmaci ha compiuto notevoli progressi negli ultimi anni. In questo contesto, i materiali polimerici rappresentano senza dubbio la tipologia più adatta: è infatti possibile modularne piuttosto facilmente le proprietà finali per ottenere materiali con caratteristiche ad hoc per il tipo di applicazione scelta, garantendo al contempo il mantenimento di biodegradabilità e biocompatibilità, essenziali in campo biomedicale. All’interno della classe dei polimeri, i poliesteri alifatici risultano particolarmente interessanti e promettenti. Tra questi ultimi, il poli(butilene succinato) (PBS) è utilizzato soprattutto nel campo degli imballaggi biodegradabili grazie alla buona stabilità termica e alla elevata temperatura di fusione (115°C). Di contro, tale polimero è caratterizzato da tempi di biodegradazione lunghi, dovuti all’elevato grado di cristallinità (circa 45-50%), nonché da proprietà meccaniche non ottimali per alcune applicazioni. In tale contesto si inserisce il presente lavoro di tesi che ha come scopo la realizzazione di nuovi poli(esteri uretani) multiblocco a base di PBS, caratterizzati da proprietà migliorate rispetto all’omopolimero di partenza. Al fine di ottenere nuovi materiali che presentino una maggiore velocità di degradazione, combinata con un comportamento meccanico sia elastomerico che termoplastico, sono state prese in considerazione due diverse unità copolimeriche: una cosiddetta “hard” e l’altra “soft”. L’alternanza di queste due porzioni permette infatti di realizzare un polimero tenace, con una elevata temperatura di fusione (dovuta all’elevato grado di cristallinità del segmento hard), e con un basso modulo elastico ed un elevato allungamento a rottura (tipici invece del segmento soft).

Novel etheroatom containing aliphatic polyesters for biomedical and environmental applications

Biodegradable polymers for short time applications have attracted much interest all over the world. The reason behind this growing interest is the incompatibility of the polymeric wastes with the environment where they are disposed after usage. Synthetic aliphatic polyesters represent one of the most economically competitive biodegradable polymers. In addition, they gained considerable attention as they combine biodegradability and biocompatibility with interesting physical and chemical properties. In this framework, the present research work focused on the modification by reactive blending and polycondensation of two different aliphatic polyesters, namely poly(butylene succinate) (PBS) and poly(butylene 1,4-cyclohexanedicarboxylate) (PBCE). Both are characterized by good thermal properties, but their mechanical characteristics do not fit the requirements for applications in which high flexibility is requested and, moreover, both show slow biodegradation rate. With the aim of developing new materials with improved characteristics with respect to the parent homopolymers, novel etheroatom containing PBS and PBCE-based fully aliphatic polyesters and copolyesters have been therefore synthesized and carefully characterized. The introduction of oxygen or sulphur atoms along the polymer chains, by acting on chemical composition or molecular architecture, tailored solid-state properties and biodegradation rate: type and amount of comonomeric units and sequence distribution deeply affected the material final properties owing, among all, to the hydrophobic/hydrophilic ratio and to the different ability of the polymer to crystallize. The versatility of the synthesized copolymers has been well proved: as a matter of fact these polymers can be exploited both for biomedical and ecological applications. Feasibility of 3D electrospun scaffolds has been investigated, biocompatibility studies and controlled release of a model molecule showed good responses. As regards ecological applications, barrier properties and eco-toxicological assessments have been conducted with outstanding results. Finally, the ability of the novel polyesters to undergo both hydrolytic and enzymatic degradation has been demonstrated under physiological and environmental conditions.

Study of a wind-wave numerical model and its integration with ocean and oil-spill numerical models

The ability to represent the transport and fate of an oil slick at the sea surface is a formidable task. By using an accurate numerical representation of oil evolution and movement in seawater, the possibility to asses and reduce the oil-spill pollution risk can be greatly improved. The blowing of the wind on the sea surface generates ocean waves, which give rise to transport of pollutants by wave-induced velocities that are known as Stokes’ Drift velocities. The Stokes’ Drift transport associated to a random gravity wave field is a function of the wave Energy Spectra that statistically fully describe it and that can be provided by a wave numerical model. Therefore, in order to perform an accurate numerical simulation of the oil motion in seawater, a coupling of the oil-spill model with a wave forecasting model is needed. In this Thesis work, the coupling of the MEDSLIK-II oil-spill numerical model with the SWAN wind-wave numerical model has been performed and tested. In order to improve the knowledge of the wind-wave model and its numerical performances, a preliminary sensitivity study to different SWAN model configuration has been carried out. The SWAN model results have been compared with the ISPRA directional buoys located at Venezia, Ancona and Monopoli and the best model settings have been detected. Then, high resolution currents provided by a relocatable model (SURF) have been used to force both the wave and the oil-spill models and its coupling with the SWAN model has been tested. The trajectories of four drifters have been simulated by using JONSWAP parametric spectra or SWAN directional-frequency energy output spectra and results have been compared with the real paths traveled by the drifters.

Metodi di composizione stragiudiziale delle controversie individuali di lavoro

L’elaborato ha ad oggetto lo studio della conciliazione e dell’arbitrato con riferimento alle controversie individuali di lavoro privato e pubblico. Vengono trattati i diversi profili che caratterizzano gli strumenti di risoluzione delle liti alternativi al processo, al fine di comprenderne la disciplina e l’effettiva portata, e di evidenziarne le criticità. L’elaborato si occupa, in primo luogo, di ricostruire il percorso di sviluppo della disciplina legislativa dei due istituti, partendo dalla configurazione del quadro della sua evoluzione storica e affrontando, poi, approfonditamente le più recenti tappe di tale evoluzione. Nella ricostruzione della disciplina della conciliazione e dell’arbitrato viene dato conto dell’assetto delle fonti, legislativa e contrattuale, definendone i rispettivi ruoli e competenze in materia: la tesi si sofferma quindi sul ruolo che il legislatore attribuisce all’autonomia collettiva e sulle modalità con le quali questo ruolo viene concretamente esercitato in sede di contrattazione. Successivamente, viene compiuta una valutazione delle conciliazioni e dell’arbitrato diretta a comprenderne l’efficacia e l’effettività. L’analisi pone in rilievo taluni elementi che sono ritenuti indispensabili per lo sviluppo delle predette caratteristiche e, quindi, per l’opzione e per la fiducia delle parti verso gli strumenti di composizione stragiudiziale delle liti. L’attenzione viene poi focalizzata sui regimi di impugnazione dei provvedimenti con cui si concludono le procedure stragiudiziali, sulla base della riflessione per la quale la diffusione di uno strumento di composizione delle controversie postula necessariamente un certo grado di stabilità degli atti che esso genera. L’ultima parte dell’elaborato è dedicata alla disamina delle ipotesi applicative di successo nell’esperienza italiana di Alternative Dispute Resolution, ossia il tentativo obbligatorio di conciliazione nei licenziamenti economici introdotto dalla Riforma Fornero, la conciliazione monocratica e l’arbitrato per l’impugnazione delle sanzioni disciplinari, anche con l’intento di comprendere quali caratteristiche ne abbiano favorito la diffusione, in rapporto alle altre tipologie di conciliazione e arbitrato di lavoro.

Climatological analysis of temperature and salinity fields in the Mediterranean sea

A climatological field is a mean gridded field that represents the monthly or seasonal trend of an ocean parameter. This instrument allows to understand the physical conditions and physical processes of the ocean water and their impact on the world climate. To construct a climatological field, it is necessary to perform a climatological analysis on an historical dataset. In this dissertation, we have constructed the temperature and salinity fields on the Mediterranean Sea using the SeaDataNet 2 dataset. The dataset contains about 140000 CTD, bottles, XBT and MBT profiles, covering the period from 1900 to 2013. The temperature and salinity climatological fields are produced by the DIVA software using a Variational Inverse Method and a Finite Element numerical technique to interpolate data on a regular grid. Our results are also compared with a previous version of climatological fields and the goodness of our climatologies is assessed, according to the goodness criteria suggested by Murphy (1993). Finally the temperature and salinity seasonal cycle for the Mediterranean Sea is described.

A study of air-sea interaction processes on water mass formation and upwelling in the Mediterranean sea

Air-sea interactions are a key process in the forcing of the ocean circulation and the climate. Water Mass Formation is a phenomenon related to extreme air-sea exchanges and heavy heat losses by the water column, being capable to transfer water properties from the surface to great depth and constituting a fundamental component of the thermohaline circulation of the ocean. Wind-driven Coastal Upwelling, on the other hand, is capable to induce intense heat gain in the water column, making this phenomenon important for climate change; further, it can have a noticeable influence on many biological pelagic ecosystems mechanisms. To study some of the fundamental characteristics of Water Mass Formation and Coastal Upwelling phenomena in the Mediterranean Sea, physical reanalysis obtained from the Mediterranean Forecating System model have been used for the period ranging from 1987 to 2012. The first chapter of this dissertation gives the basic description of the Mediterranean Sea circulation, the MFS model implementation, and the air-sea interaction physics. In the second chapter, the problem of Water Mass Formation in the Mediterranean Sea is approached, also performing ad-hoc numerical simulations to study heat balance components. The third chapter considers the study of Mediterranean Coastal Upwelling in some particular areas (Sicily, Gulf of Lion, Aegean Sea) of the Mediterranean Basin, together with the introduction of a new Upwelling Index to characterize and predict upwelling features using only surface estimates of air-sea fluxes. Our conclusions are that latent heat flux is the driving air-sea heat balance component in the Water Mass Formation phenomenon, while sensible heat exchanges are fundamental in Coastal Upwelling process. It is shown that our upwelling index is capable to reproduce the vertical velocity patterns in Coastal Upwelling areas. Nondimensional Marshall numbers evaluations for the open-ocean convection process in the Gulf of Lion show that it is a fully turbulent, three-dimensional phenomenon.

Nuovi elastomeri termoplastici "soft-hard" a base di pbs per applicazioni biomedicali

Nuovi elastomeri termoplastici "soft-hard" a base di PBS per applicazioni biomedicali

Nuovi copoliesteri multiblocco bio-based per applicazioni biomedicali: Correlazioni proprieta-struttura.

Sintesi e caratterizzazione di nuovi poliesteri alifatici per uso biomedicale.

Proposta di sottotitolaggio della serie tv "los quien"

L'obiettivo di questo progetto è stato il sottotitolaggio del primo episodio della sitcom spagnola "Los Quién". Nel primo capitolo viene presentata la traduzione audiovisiva e diverse tecniche di trasferimento del linguaggio per i prodotti audiovisivi, in particolare viene approfondito il sottotitolaggio e le sue caratteristiche. Il secondo capitolo è dedicato all'ampliamento sulle fiction e sulle sitcom, presentando, inoltre, la serie e i personaggi. Il terzo capitolo presenta la proposta di sottotitolaggio. Il quarto e ultimo capitolo si concentra sull'analisi delle diverse difficoltà linguistiche incontrate e il commento sulle strategie traduttive adottate.

Observations and modeling of the Marginal Ice Zone

Global climate change in recent decades has strongly influenced the Arctic generating pronounced warming accompanied by significant reduction of sea ice in seasonally ice-covered seas and a dramatic increase of open water regions exposed to wind [Stephenson et al., 2011]. By strongly scattering the wave energy, thick multiyear ice prevents swell from penetrating deeply into the Arctic pack ice. However, with the recent changes affecting Arctic sea ice, waves gain more energy from the extended fetch and can therefore penetrate further into the pack ice. Arctic sea ice also appears weaker during melt season, extending the transition zone between thick multi-year ice and the open ocean. This region is called the Marginal Ice Zone (MIZ). In the Arctic, the MIZ is mainly encountered in the marginal seas, such as the Nordic Seas, the Barents Sea, the Beaufort Sea and the Labrador Sea. Formed by numerous blocks of sea ice of various diameters (floes) the MIZ, under certain conditions, allows maritime transportation stimulating dreams of industrial and touristic exploitation of these regions and possibly allowing, in the next future, a maritime connection between the Atlantic and the Pacific. With the increasing human presence in the Arctic, waves pose security and safety issues. As marginal seas are targeted for oil and gas exploitation, understanding and predicting ocean waves and their effects on sea ice become crucial for structure design and for real time safety of operations. The juxtaposition of waves and sea ice represents a risk for personnel and equipment deployed on ice, and may complicate critical operations such as platform evacuations. The risk is difficult to evaluate because there are no long-term observations of waves in ice, swell events are difficult to predict from local conditions, ice breakup can occur on very short time-scales and wave-ice interactions are beyond the scope of current forecasting models [Liu and Mollo-Christensen, 1988,Marko, 2003]. In this thesis, a newly developed Waves in Ice Model (WIM) [Williams et al., 2013a,Williams et al., 2013b] and its related Ocean and Sea Ice model (OSIM) will be used to study the MIZ and the improvements of wave modeling in ice infested waters. The following work has been conducted in collaboration with the Nansen Environmental and Remote Sensing Center and within the SWARP project which aims to extend operational services supporting human activity in the Arctic by including forecast of waves in ice-covered seas, forecast of sea-ice in the presence of waves and remote sensing of both waves and sea ice conditions. The WIM will be included in the downstream forecasting services provided by Copernicus marine environment monitoring service.

Il modello geotecnico del sottosuolo dei comuni costieri da Cesenatico (FC) a Bellaria-Igea Marina (RN).

La presente tesi descrive la messa a punto del modello geotecnico del sottosuolo di una zona dell’Emilia-Romagna che comprende i Comuni di Cesenatico, Gatteo, San Mauro Pascoli, Savignano sul Rubicone e Bellaria-Igea Marina. Il modello si basa principalmente sull'interpretazione delle misure da prove penetrometriche statiche con piezocono e dei sondaggi, unitamente ad un più limitato numero di prove di laboratorio. Nella prima parte della tesi si descrive la geologia dell'area e si illustra il database sperimentale disponibile. Nella seconda parte sono invece analizzate nel dettaglio le prove ai fini della individuazione delle unità stratigrafiche presenti e della successiva caratterizzazione meccanica delle stesse. Il modello è stato costruito in diverse fasi. Nella prima fase sono state elaborate le singole prove penetrometriche: utilizzando approcci interpretativi noti, per lo più di tipo empirico, si è proceduto a classificare i terreni attraversati, sono state preliminarmente individuate alcune le unità stratigrafiche presenti e ad esse sono stati assegnati valori rappresentativi dei parametri meccanici di interesse. Successivamente si è proceduto ad una sintesi delle informazioni e dei risultati conseguiti per le singole verticali di analisi, facendo riferimento ad un certo numero di sezioni longitudinali e trasversali ritenute più significative. In questo modo è stato possibile costruire un modello geotecnico alla scala territoriale, con l'obiettivo non solo di fornire uno strumento utile in una fase preliminare della progettazione geotecnica, ma anche di indirizzare il progettista nell’ottimizzazione delle prove da programmare e nella scelta delle procedure interpretative più idonee per la stima dei parametri meccanici.