Atmospheric radiative transfer in multiple scattering conditions. Application to NWP models.

High spectral resolution radiative transfer (RT) codes are essential tools in the study of the radiative energy transfer in the Earth atmosphere and a support for the development of parameterizations for fast RT codes used in climate and weather prediction models. Cirrus clouds cover permanently 30% of the Earth's surface, representing an important contribution to the Earth-atmosphere radiation balance. The work has been focussed on the development of the RT model LBLMS. The model, widely tested in the infra-red spectral range, has been extended to the short wave spectrum and it has been used in comparison with airborne and satellite measurements to study the optical properties of cirrus clouds. A new database of single scattering properties has been developed for mid latitude cirrus clouds. Ice clouds are treated as a mixture of ice crystals with various habits. The optical properties of the mixture are tested in comparison to radiometric measurements in selected case studies. Finally, a parameterization of the mixture for application to weather prediction and global circulation models has been developed. The bulk optical properties of ice crystals are parameterized as functions of the effective dimension of measured particle size distributions that are representative of mid latitude cirrus clouds. Tests with the Limited Area Weather Prediction model COSMO have shown the impact of the new parameterization with respect to cirrus cloud optical properties based on ice spheres.

Astronomical site testing in the era of the extremely large telescopes

The quality of astronomical sites is the first step to be considered to have the best performances from the telescopes. In particular, the efficiency of large telescopes in UV, IR, radio etc. is critically dependent on atmospheric transparency. It is well known that the random optical effects induced on the light propagation by turbulent atmosphere also limit telescope’s performances. Nowadays, clear appears the importance to correlate the main atmospheric physical parameters with the optical quality reachable by large aperture telescopes. The sky quality evaluation improved with the introduction of new techniques, new instrumentations and with the understanding of the link between the meteorological (or synoptical parameters and the observational conditions thanks to the application of the theories of electromagnetic waves propagation in turbulent medias: what we actually call astroclimatology. At the present the site campaigns are evolved and are performed using the classical scheme of optical seeing properties, meteorological parameters, sky transparency, sky darkness and cloudiness. New concept are added and are related to the geophysical properties such as seismicity, microseismicity, local variability of the climate, atmospheric conditions related to the ground optical turbulence and ground wind regimes, aerosol presence, use of satellite data. The purpose of this project is to provide reliable methods to analyze the atmospheric properties that affect ground-based optical astronomical observations and to correlate them with the main atmospheric parameters generating turbulence and affecting the photometric accuracy. The first part of the research concerns the analysis and interpretation of longand short-time scale meteorological data at two of the most important astronomical sites located in very different environments: the Paranal Observatory in the Atacama Desert (Chile), and the Observatorio del Roque de Los Muchachos(ORM) located in La Palma (Canary Islands, Spain). The optical properties of airborne dust at ORM have been investigated collecting outdoor data using a ground-based dust monitor. Because of its dryness, Paranal is a suitable observatory for near-IR observations, thus the extinction properties in the spectral range 1.00-2.30 um have been investigated using an empirical method. Furthermore, this PhD research has been developed using several turbulence profilers in the selection of the site for the European Extremely Large Telescope(E-ELT). During the campaigns the properties of the turbulence at different heights at Paranal and in the sites located in northern Chile and Argentina have been studied. This given the possibility to characterize the surface layer turbulence at Paranal and its connection with local meteorological conditions.

Slope stability analysis by multi-temporal DEMs and 3D modelling: The 2002 and 2007 Stromboli landslide events

Natural hazard related to the volcanic activity represents a potential risk factor, particularly in the vicinity of human settlements. Besides to the risk related to the explosive and effusive activity, the instability of volcanic edifices may develop into large landslides often catastrophically destructive, as shown by the collapse of the northern flank of Mount St. Helens in 1980. A combined approach was applied to analyse slope failures that occurred at Stromboli volcano. SdF slope stability was evaluated by using high-resolution multi-temporal DTMMs and performing limit equilibrium stability analyses. High-resolution topographical data collected with remote sensing techniques and three-dimensional slope stability analysis play a key role in understanding instability mechanism and the related risks. Analyses carried out on the 2002–2003 and 2007 Stromboli eruptions, starting from high-resolution data acquired through airborne remote sensing surveys, permitted the estimation of the lava volumes emplaced on the SdF slope and contributed to the investigation of the link between magma emission and slope instabilities. Limit Equilibrium analyses were performed on the 2001 and 2007 3D models, in order to simulate the slope behavior before 2002-2003 landslide event and after the 2007 eruption. Stability analyses were conducted to understand the mechanisms that controlled the slope deformations which occurred shortly after the 2007 eruption onset, involving the upper part of slope. Limit equilibrium analyses applied to both cases yielded results which are congruent with observations and monitoring data. The results presented in this work undoubtedly indicate that hazard assessment for the island of Stromboli should take into account the fact that a new magma intrusion could lead to further destabilisation of the slope, which may be more significant than the one recently observed because it will affect an already disarranged deposit and fractured and loosened crater area. The two-pronged approach based on the analysis of 3D multi-temporal mapping datasets and on the application of LE methods contributed to better understanding volcano flank behaviour and to be prepared to undertake actions aimed at risk mitigation.

Il monitoraggio suolo-pianta per la valutazione dell'inquinamento da metalli pesanti nell'ambiente urbano

Il lavoro di tesi è incentrato sulla valutazione del degrado del suolo dovuto a fenomeni di inquinamento da metalli pesanti aerodispersi, ovvero apportati al suolo mediante deposizioni atmosferiche secche ed umide, in ambiente urbano. Lo scopo della ricerca è legato principalmente alla valutazione dell’efficienza del metodo di monitoraggio ideato che affianca al campionamento e all’analisi pedologica l’utilizzo di bioindicatori indigeni, quali il muschio, il cotico erboso, le foglie di piante arboree e il materiale pulverulento depositatosi su di esse. Una semplice analisi pedologica infatti non permette di discriminare la natura dei contaminanti in esso ritrovati. I metalli pesanti possono raggiungere il suolo attraverso diverse vie. In primo luogo questi elementi in traccia si trovano naturalmente nei suoi; ma numerose sono le fonti antropiche: attività industriali, traffico veicolare, incenerimento dei rifiuti, impianti di riscaldamento domestico, pratiche agricole, utilizzo di acque con bassi requisiti di qualità, ecc. Questo fa capire come una semplice analisi del contenuto totale o pseudo - totale di metalli pesanti nel suolo non riesca a rispondere alla domanda su quale si la fonte di provenienza di queste sostanze. Il metodo di monitoraggio integrato suolo- pianta è stato applicato a due diversi casi di studio. Il primo denominato “Progetto per il monitoraggio e valutazione delle concentrazioni in metalli pesanti e micro elementi sul sistema suolo - pianta in aree urbane adibite a verde pubblico dell’Emilia – Romagna” ha permesso di valutare l’insorgenza di una diminuzione della qualità dell’ecosistema parco urbano causata dalla ricaduta di metalli pesanti aerotrasportati, in tre differenti realtà urbane dell’Emilia Romagna: le città di Bologna, Ferrara e Cesena. Le città presentano caratteristiche pedologiche, ambientali ed economico-sociali molto diverse tra loro. Questo ha permesso di studiare l’efficienza del metodo su campioni di suolo e di vegetali molto diversi per quanto riguarda le aliquote di metalli pesanti riscontrate. Il secondo caso di studio il “Monitoraggio relativo al contenuto in metalli pesanti e microelementi nel sistema acqua-suolo-pianta delle aree circostanti l’impianto di termovalorizzazione e di incenerimento del Frullo (Granarolo dell’Emilia - BO)” è stato invece incentrato sulla valutazione della qualità ambientale delle aree circostanti l’inceneritore. Qui lo scenario si presentava più omogeneo dal punto di vista pedologico rispetto al caso di studio precedente, ma molto più complesso l’ecosistema di riferimento (urbano, extra-urbano ed agricolo). Seppure il metodo suolo-pianta abbia permesso di valutare gli apporti di metalli pesanti introdotti per via atmosferica, non è stato possibile imputarne l’origine alle sole emissioni prodotte dall’inceneritore.

Novel techniques for the remote sensing of photosynthetic processes

Remote sensing (RS) techniques have evolved into an important instrument to investigate forest function. New methods based on the remote detection of leaf biochemistry and photosynthesis are being developed and applied in pilot studies from airborne and satellite platforms (PRI, solar-induced fluorescence; N and chlorophyll content). Non-destructive monitoring methods, a direct application of RS studies, are also proving increasingly attractive for the determination of stress conditions or nutrient deficiencies not only in research but also in agronomy, horticulture and urban forestry (proximal RS). In this work I will focus on some novel techniques recently developed for the estimation of photochemistry and photosynthetic rates based (i) on the proximal measurement of steady-state chlorophyll fluorescence yield, or (ii) the remote sensing of changes in hyperspectral leaf reflectance, associated to xanthophyll de-epoxydation and energy partitioning, which is closely coupled to leaf photochemistry and photosynthesis. I will also present and describe a mathematical model of leaf steady-state fluorescence and photosynthesis recently developed in our group. Two different species were used in the experiments: Arbutus unedo, a schlerophyllous Mediterranean species, and Populus euroamericana, a broad leaf deciduous tree widely used in plantation forestry. Results show that ambient fluorescence could provide a useful tool for testing photosynthetic processes from a distance. These results confirm also the photosynthetic reflectance index (PRI) as an efficient remote sensing reflectance index estimating short-term changes in photochemical efficiency as well as long-term changes in leaf biochemistry. The study also demonstrated that RS techniques could provide a fast and reliable method to estimate photosynthetic pigment content and total nitrogen, beside assessing the state of photochemical process in our plants’ leaves in the field. This could have important practical applications for the management of plant cultivation systems, for the estimation of the nutrient requirements of our plants for optimal growth.

Analisi del profilo tossicologico e cancerogeno del particolato atmosferico e identificazione dei rischi per la salute umana correlati all'esposizione

Gli impianti di incenerimento di rifiuti solidi suscitano preoccupazione nella popolazione per i possibili effetti avversi associati all’esposizione. Gli effetti delle polveri sottili (PM2.5), generate dai processi di combustione, sulla salute umana includono l’insorgenza di patologie a carico del sistema respiratorio e cardiovascolare e l’aumento della mortalità per malattie polmonari e probabilmente cancro al polmone. Lo scopo della tesi è quello di valutare il profilo tossicologico e cancerogeno del particolato atmosferico in prossimità dell’inceneritore di Bologna rispetto alle aree adiacenti mediante l’utilizzo di test alternativi alle metodologie in vivo, come il test di trasformazione cellulare e approcci di tossicogenomica (soprattutto trascrittomica) oltre alla valutazione della variazione del rischio cancerogeno indotto dall’esposizione di PM2.5 in diversi siti (massima ricaduta, controllo, fondo urbano e fondo rurale) e in differenti periodi di campionamento (estate 2008 e inverno 2009). Gli estratti di PM2.5 relativi alla stagione invernale sono risultati più tossici rispetto ai campioni estivi, che inducono tossicità soprattutto alle alte dosi. Per i campioni invernali il numero medio di colonie di cellule BALB/c 3T3 A31-1-1 risulta ridotto in modo significativo anche per le dosi più basse saggiate indipendentemente dal sito di provenienza. Tutti i campioni analizzati sono risultati negativi nel test di trasformazione cellulare in vitro. L’analisi dell’espressione genica delle cellule BALB/c 3T3 A31-1-1, in seguito all’esposizione agli estratti di PM2.5, ha mostrato un effetto stagionale evidente. Relativamente ai campioni invernali è stato evidenziato un maggior effetto tossico da parte del sito di controllo rispetto alla massima ricaduta, poiché nel sito di controllo risultano attivati marcatori di morte cellulare per apoptosi. La valutazione del rischio cancerogeno in tutti i siti valutati non mostra situazioni preoccupanti legate alla predizione di eccessi di rischio di tumori imputabili all’attività dell’inceneritore in quanto le stime di rischio non eccedono mai il valore limite riportato in letteratura.

Indoor and Outdoor Natural Radioactivity in the Vulsini Volcanic District (Central Italy): Estimation of Doses and Radiological Risks

Terrestrial radioactivity for most individual is the major contributor to the total dose and is mostly provided by 238U, 232Th and 40K radionuclides. In particular indoor radioactivity is principally due to 222Rn, a radioactive noble gas descendent of 238U, second cause of lung cancer after cigarettes smoking. Vulsini Volcanic District is a well known quaternary volcanic area located between the northern Latium and southern Tuscany (Central Italy). It is characterized by an high natural radiation background resulting from the high concentrations of 238U, 232Th and 40K in the volcanic products. In this context, subduction-related metasomatic enrichment of incompatible elements in the mantle source coupled with magma differentiation within the upper crust has given rise to U, Th and K enriched melts. Almost every ancient village and town located in this part of Italy has been built with volcanic rocks pertaining to the Vulsini Volcanic District. The radiological risk of living in this area has been estimated considering separately: a. the risk associated with buildings made of volcanic products and built on volcanic rock substrates b. the risk associated to soil characteristics. The former has been evaluated both using direct 222Rn indoor measurements and simulations of “standard rooms” built with the tuffs and lavas from the Vulsini Volcanic District investigated in this work. The latter has been carried out by using in situ measurements of 222Rn activity in the soil gases. A radon risk map for the Bolsena village has been developed using soil radon measurements integrating geological information. Data of airborne radioactivity in ambient aerosol at two elevated stations in Emilia Romagna (North Italy) under the influence of Fukushima plume have been collected, effective doses have been calculated and an extensive comparison between doses associated with artificial and natural sources in different area have been described and discussed.

New techniques for the remote sensing of foliar nitrogen concentration in forest ecosystems.

During my Doctoral study I researched about the remote detection of canopy N concentration in forest stands, its potentials and problems, under many overlapping perspectives. The study consisted of three parts. In S. Rossore 2000 dataset analysis, I tested regressions between N concentration and NIR reflectances derived from different sources (field samples, airborne and satellite sensors). The analysis was further expanded using a larger dataset acquired in year 2009 as part of a new campaign funded by the ESA. In both cases, a good correlation was observed between Landsat NIR, using both TM (2009) and ETM+ (2000) imagery, and N concentration measured by a CHN elemental analyzer. Concerning airborne sensors I did not obtain the same good results, mainly because of the large FOV of the two instruments, and to the anisotropy of vegetation reflectance. We also tested the relation between ground based ASD measures and nitrogen concentration, obtaining really good results. Thus, I decided to expand my study to the regional level, focusing only on field and satellite measures. I analyzed a large dataset for the whole of Catalonia, Spain; MODIS imagery was used, in consideration of its spectral characteristics and despite its rather poor spatial resolution. Also in this case a regression between nitrogen concentration and reflectances was found, but not so good as in previous experiences. Moreover, vegetation type was found to play an important role in the observed relationship. We concluded that MODIS is not the most suitable satellite sensor in realities like Italy and Catalonia, which present a patchy and inhomogeneous vegetation cover; so it could be utilized for the parameterization of eco-physiological and biogeochemical models, but not for really local nitrogen estimate. Thus multispectral sensors similar to Landsat Thematic Mapper, with better spatial resolution, could be the most appropriate sensors to estimate N concentration.

Advanced modelling of time domain electromagnetic data with updated hydrogeological interpretations

Several countries have acquired, over the past decades, large amounts of area covering Airborne Electromagnetic data. Contribution of airborne geophysics has dramatically increased for both groundwater resource mapping and management proving how those systems are appropriate for large-scale and efficient groundwater surveying. We start with processing and inversion of two AEM dataset from two different systems collected over the Spiritwood Valley Aquifer area, Manitoba, Canada respectively, the AeroTEM III (commissioned by the Geological Survey of Canada in 2010) and the “Full waveform VTEM” dataset, collected and tested over the same survey area, during the fall 2011. We demonstrate that in the presence of multiple datasets, either AEM and ground data, due processing, inversion, post-processing, data integration and data calibration is the proper approach capable of providing reliable and consistent resistivity models. Our approach can be of interest to many end users, ranging from Geological Surveys, Universities to Private Companies, which are often proprietary of large geophysical databases to be interpreted for geological and\or hydrogeological purposes. In this study we deeply investigate the role of integration of several complimentary types of geophysical data collected over the same survey area. We show that data integration can improve inversions, reduce ambiguity and deliver high resolution results. We further attempt to use the final, most reliable output resistivity models as a solid basis for building a knowledge-driven 3D geological voxel-based model. A voxel approach allows a quantitative understanding of the hydrogeological setting of the area, and it can be further used to estimate the aquifers volumes (i.e. potential amount of groundwater resources) as well as hydrogeological flow model prediction. In addition, we investigated the impact of an AEM dataset towards hydrogeological mapping and 3D hydrogeological modeling, comparing it to having only a ground based TEM dataset and\or to having only boreholes data.