Tecniche Cloud Avanzate per Adaptive Hadoop Load Balancing tramite Sahara

Ogni giorno vengono generati grandi moli di dati attraverso sorgenti diverse. Questi dati, chiamati Big Data, sono attualmente oggetto di forte interesse nel settore IT (Information Technology). I processi digitalizzati, le interazioni sui social media, i sensori ed i sistemi mobili, che utilizziamo quotidianamente, sono solo un piccolo sottoinsieme di tutte le fonti che contribuiscono alla produzione di questi dati. Per poter analizzare ed estrarre informazioni da questi grandi volumi di dati, tante sono le tecnologie che sono state sviluppate. Molte di queste sfruttano approcci distribuiti e paralleli. Una delle tecnologie che ha avuto maggior successo nel processamento dei Big Data, e Apache Hadoop. Il Cloud Computing, in particolare le soluzioni che seguono il modello IaaS (Infrastructure as a Service), forniscono un valido strumento all'approvvigionamento di risorse in maniera semplice e veloce. Per questo motivo, in questa proposta, viene utilizzato OpenStack come piattaforma IaaS. Grazie all'integrazione delle tecnologie OpenStack e Hadoop, attraverso Sahara, si riesce a sfruttare le potenzialita offerte da un ambiente cloud per migliorare le prestazioni dell'elaborazione distribuita e parallela. Lo scopo di questo lavoro e ottenere una miglior distribuzione delle risorse utilizzate nel sistema cloud con obiettivi di load balancing. Per raggiungere questi obiettivi, si sono rese necessarie modifiche sia al framework Hadoop che al progetto Sahara.

Idrochimica delle acque interstiziali e scambi acqua / sedimento nell'invaso di Ridracoli

Uno degli aspetti più influenti sulla qualità chimica e biologica dell’acqua di laghi e invasi, caratteristico del bacino di Ridracoli, è rappresentato dalla stratificazione termica, un processo di formazione di volumi d’acqua a diversa densità che può verificarsi allorquando, in alcune circostanze e, nello specifico, durante la stagione estiva, si instauri una condizione stabile in cui l’acqua riscaldata dalla radiazione solare sovrasta quella più fredda e densa del fondo. Una delle conseguenze di tali variazioni termiche è che esse inducono cambiamenti nei livelli di ossigeno disciolto, favorendo l’instaurarsi di processi di degradazione anaerobica della materia organica e determinando la formazione di un chimismo ostile per l’attività biologica. I cicli stagionali, redox-dipendenti, di Ferro e Manganese tra la colonna d’acqua e i sedimenti sono caratteristici di questi ambienti ed una loro risospensione in forma disciolta è stato rilevato nell’ipolimnio dell’invaso di Ridracoli, stagionalmente anossico. Questo studio, collocato all’interno di un ampio progetto finanziato da Romagna Acque Società delle Fonti S.p.A. con la Facoltà di Scienze Ambientali – Campus di Ravenna ed il CNR-ISMAR, si è posto come obiettivo l’individuazione dei fattori che controllano la distribuzione e la mobilità degli elementi chimici all’interno del sistema acqua-sedimento dell’invaso di Ridracoli ed è articolato in tre diverse fasi: • Indagine della composizione chimica del sedimento; • Analisi ed interpretazione della composizione chimica delle acque interstiziali • Stima del flussi attraverso l’interfaccia acqua-sedimento mediante l’utilizzo di una camera bentica e l’applicazione della prima legge di Fick sulla diffusione. Al termine del lavoro è stato possibile ricostruire un quadro diagenetico generale contraddistinto da una deplezione degli accettori di elettroni principali (O2 e NO3-) entro i primi millimetri di sedimento, da un consumo immediato di SO42- e da una graduale riduzione degli ossidi di Mn (IV) e Fe (III), con formazione di gradienti negativi ed il rilascio di sostanze disciolte nella colonna d’acqua.

Eine Karriere im Schatten von Rosalba Carriera. Felicita Sartori / Hoffmann in Venedig und Dresden

Felicita Sartori, nata a Pordenone nel 1714 ca. come figlia del notaio Felice Sartori e di Tommasa Scotti, ricevette la sua prima formazione artistica intorno al 1724 da suo zio, il calcografo Antonio dall'Agata a Gorizia. Tramite lo zio la quattordicenne si trasferisce a Venezia dove entra nella bottega-casa di Rosalba Carriera per perfezionarsi nella miniatura e nella pittura a pastello senoché nelle varie tecniche della grafica. Durante gli anni seguenti Felicita diventa, accanto alle sorelle di Rosalba, la collaboratrice piú stretta della Carriera che in questi anni tocca il colmo della fama artistica, dovuto soprattutto al suo strepitoso successo riscosso durante il soggiorno a Parigi dal 1720 al 1721. I numerosissimi incarichi che le giungono da tutta l'Europa incrementano la produttivitá e lasciano supporre che la bottega abbia contribuito in misura notevole a contentare tali richieste. Negli anni dopo il 1730 l'attività di Felicita oltre le varie attività pittoriche entro la bottega della Carriera si estende alla produzione di incisioni per le pubblicazioni di Gaspare Stampa e di Jacques-Bénigne Bossuet. Incide inoltre le stampe dai disegni di Giovanni Battista Piazetta, pubblicati da Antonio Maria Zanetti. La finora anonima collaboratrice della famosa veneziana esce dall'ombra quando, nel 1741, viene nominata artista di corte da Augusto III, principe elettore di Sassonia e ré di Polonia. Trasferitosi a Dresda, si unisce poche settimane dopo la nomina in matrimonio al consigliere di corte Franz Joseph von Hoffmann, che probabilmente aveva concosciuto nel 1740 nello studio veneziano di Rosalba spesso frequentato dall'elettore e del suo seguito. Felicita continua la su attività a Dresda dove nella Gemäldegalerie Alte Meister si conservano tuttora 15 miniature di sua mano. Grazie alle ricerche dedicate a queste opere è stato possibile di aumentare l'œuvre della Sartori di altre opere tra cui una Betsabea al bagno (coll. priv. München) già nelle collezioni reali sassoni. Sembra che l'artista dopo la morte del marito nel 1749, si sia trasferito con un secondo marito a Bamberg ma altre fonti citano la sua presenza a Dresda nel 1753 dove secondo le notizie fornite da Jean Pierre Mariette muore nel 1760 all'età di soli 46 anni.

Tree growth response along an elevational gradient: climate or genetics?

Environment and genetics combine to influence tree growth and should therefore be jointly considered when evaluating forest responses in a warming climate. Here, we combine dendroclimatology and population genetic approaches with the aim of attributing climatic influences on growth of European larch (Larix decidua) and Norway spruce (Picea abies). Increment cores and genomic DNA samples were collected from populations along a ~900-m elevational transect where the air temperature gradient encompasses a ~4 °C temperature difference. We found that low genetic differentiation among populations indicates gene flow is high, suggesting that migration rate is high enough to counteract the selective pressures of local environmental variation. We observed lower growth rates towards higher elevations and a transition from negative to positive correlations with growing season temperature upward along the elevational transect. With increasing elevation there was also a clear increase in the explained variance of growth due to summer temperatures. Comparisons between climate sensitivity patterns observed along this elevational transect with those from Larix and Picea sites distributed across the Alps reveal good agreement, and suggest that tree-ring width (TRW) variations are more climate-driven than genetics-driven at regional and larger scales. We conclude that elevational transects are an extremely valuable platform for understanding climatic-driven changes over time and can be especially powerful when working within an assessed genetic framework.

A meta-analysis of cambium phenology and growth: linear and non-linear patterns in conifers of the northern hemisphere

Background and Aims Ongoing global warming has been implicated in shifting phenological patterns such as the timing and duration of the growing season across a wide variety of ecosystems. Linear models are routinely used to extrapolate these observed shifts in phenology into the future and to estimate changes in associated ecosystem properties such as net primary productivity. Yet, in nature, linear relationships may be special cases. Biological processes frequently follow more complex, non-linear patterns according to limiting factors that generate shifts and discontinuities, or contain thresholds beyond which responses change abruptly. This study investigates to what extent cambium phenology is associated with xylem growth and differentiation across conifer species of the northern hemisphere. Methods Xylem cell production is compared with the periods of cambial activity and cell differentiation assessed on a weekly time scale on histological sections of cambium and wood tissue collected from the stems of nine species in Canada and Europe over 1–9 years per site from 1998 to 2011. Key Results The dynamics of xylogenesis were surprisingly homogeneous among conifer species, although dispersions from the average were obviously observed. Within the range analysed, the relationships between the phenological timings were linear, with several slopes showing values close to or not statistically different from 1. The relationships between the phenological timings and cell production were distinctly non-linear, and involved an exponential pattern. Conclusions The trees adjust their phenological timings according to linear patterns. Thus, shifts of one phenological phase are associated with synchronous and comparable shifts of the successive phases. However, small increases in the duration of xylogenesis could correspond to a substantial increase in cell production. The findings suggest that the length of the growing season and the resulting amount of growth could respond differently to changes in environmental conditions.

Intra-annual dynamics of non-structural carbohydrates in the cambium of mature conifer trees reflects radial growth demands

The presence of soluble carbohydrates in the cambial zone, either from sugars recently produced during photosynthesis or from starch remobilized from storage organs, is necessary for radial tree growth. However, considerable uncertainties on carbohydrate dynamics and the consequences on tree productivity exist. This study aims to better understand the variation in different carbon pools at intra-annual resolution by quantifying how cambial zone sugar and starch concentrations fluctuate over the season and in relation to cambial phenology. A comparison between two physiologically different species growing at the same site, i.e., the evergreen Picea abies Karst. and the deciduous Larix decidua Mill., and between L. decidua from two contrasting elevations, is presented to identify mechanisms of growth limitation. Results indicate that the annual cycle of sugar concentration within the cambial zone is coupled to the process of wood formation. The highest sugar concentration is observed when the number of cells in secondary wall formation and lignification stages is at a maximum, subsequent to most radial growth. Starch disappears in winter, while other freeze-resistant non-structural carbohydrates (NSCs) increase. Slight differences in NSC concentration between species are consistent with the differing climate sensitivity of the evergreen and deciduous species investigated. The general absence of differences between elevations suggests that the cambial activity of trees growing at the treeline was not limited by the availability of carbohydrates at the cambial zone but instead by environmental controls on the growing season duration.

Climatic drivers of hourly to yearly tree radius variations along a 6°C natural warming gradient

Climate affects the timing, rate and dynamics of tree growth, over time scales ranging from seconds to centuries. Monitoring how a tree's stem radius varies over these time scales can provide insight into intra-annual stem dynamics and improve our understanding of climate impacts on tree physiology and growth processes. Here, we quantify the response of radial conifer stem size to environmental fluctuations via a novel assessment of tree circadian cycles. We analyze four years of sub-hourly data collected from 56 larch and spruce trees growing along a natural temperature gradient of ∼6 °C in the central Swiss Alps. During the growing season, tree stem diameters were greatest at mid-morning and smallest in the late evening, reflecting the daily cycle of water uptake and loss. Along the gradient, amplitudes calculated from the stem radius cycle were ∼50% smaller at the upper site (∼2200 m a.s.l.) relative to the lower site (∼800 m a.s.l.). We show changes in precipitation, temperature and cloud cover have a substantial effect on typical growing season diurnal cycles; amplitudes were nine times smaller on rainy days (>10 mm), and daily amplitudes are approximately 40% larger when the mean daily temperature is 15–20 °C than when it is 5–10 °C. We find that over the growing season in the sub-alpine forests, spruce show greater daily stem water movement than larch. However, under projected future warming, larch could experience up to 50% greater stem water use, which may severely affect future growth on already dry sites. Our data further indicate that because of the confounding influences of radial growth and short-term water dynamics on stem size, conventional methodology probably overstates the effect of water-linked meteorological variables (i.e. precipitation and relative humidity) on intra-annual tree growth. We suggest future studies use intra-seasonal measurements of cell development and consider whether climatic factors produce reversible changes in stem diameter. These study design elements may help researchers more accurately quantify and attribute changes in forest productivity in response to future warming.

Climate sensitivity of Mediterranean pine growth reveals distinct east-west dipole

The European Mediterranean region is governed by a characteristic climate of summer drought that is likely to increase in duration and intensity under predicted climate change. However, large-scale network analyses investigating spatial aspects of pre-instrumental drought variability for this biogeographic zone are still scarce. In this study we introduce 54 mid- to high-elevation tree-ring width (TRW) chronologies comprising 2186 individual series from pine trees (Pinus spp.). This compilation spans a 4000-km east–west transect from Spain to Turkey, and was subjected to quality control and standardization prior to the development of site chronologies. A principal component analysis (PCA) was applied to identify spatial growth patterns during the network's common period 1862–1976, and new composite TRW chronologies were developed and investigated. The PCA reveals a common variance of 19.7% over the 54 Mediterranean pine chronologies. More interestingly, a dipole pattern in growth variability is found between the western (15% explained variance) and eastern (9.6%) sites, persisting back to 1330 AD. Pine growth on the Iberian Peninsula and Italy favours warm early growing seasons, but summer drought is most critical for ring width formation in the eastern Mediterranean region. Synoptic climate dynamics that have been in operation for the last seven centuries have been identified as the driving mechanism of a distinct east–west dipole in the growth variability of Mediterranean pines.

Intra-annual patterns of tracheid size in the Mediterranean tree Juniperus thurifera as an indicator of seasonal water stress

Because climate can affect xylem cell anatomy, series of intra-annual cell anatomical features have the potential to retrospectively supply seasonal climatic information. In this study, we explored the ability to extract information about water stress conditions from tracheid features of the Mediterranean conifer Juniperus thurifera L. Tracheidograms of four climatic years from two drought-sensitive sites in Spain were compared to evaluate whether it is possible to link intra-annual cell size patterns to seasonal climatic conditions. Results indicated site-specific anatomical adjustment such as smaller and thicker tracheids at the dryer site but also showed a strong climatic imprint on the intra-annual pattern of tracheid size. Site differences in cell size reflected expected structural adjustments against cavitation failures. Differences between intra-annual patterns, however, indicated a response to seasonal changes in water availability whereby cells formed under drought conditions were smaller and thicker, and vice versa. This relationship was more manifest and stable at the dryer site