Luminosity determination for the measurement of the proton-proton total cross section at 8 TeV in the Atlas experiment

La sezione d’urto totale adronica gioca un ruolo fondamentale nel programma di fisica di LHC. Un calcolo di questo parametro, fondamentale nell’ambito della teoria delle interazioni forti, non é possibile a causa dell’inapplicabilità dell’approccio perturbativo. Nonostante ciò, la sezione d’urto può essere stimata, o quanto meno le può essere dato un limite, grazie ad un certo numero di relazioni, come ad esempio il Teorema Ottico. In questo contesto, il detector ALFA (An Absolute Luminosity For ATLAS) sfrutta il Teorema Ottico per determinare la sezione d’urto totale misurando il rate di eventi elastici nella direzione forward. Un tale approccio richiede un metodo accurato di misura della luminosità in condizioni sperimentali difficoltose, caratterizzate da valori di luminosità istantanea inferiore fino a 7 ordini di grandezza rispetto alle normali condizioni di LHC. Lo scopo di questa tesi è la determinazione della luminosità integrata di due run ad alto β*, utilizzando diversi algoritmi di tipo Event-Counting dei detector BCM e LUCID. Particolare attenzione è stata riservata alla sottrazione del fondo e allo studio delle in- certezze sistematiche. I valori di luminosità integrata ottenuti sono L = 498.55 ± 0.31 (stat) ± 16.23 (sys) μb^(-1) and L = 21.93 ± 0.07 (stat) ± 0.79 (sys) μb^(-1), rispettivamente per i due run. Tali saranno forniti alla comunità di fisica che si occupa della misura delle sezioni d’urto protone-protone, elastica e totale. Nel Run II di LHC, la sezione d’urto totale protone-protone sarà stimata con un’energia nel centro di massa di 13 TeV per capire meglio la sua dipendenza dall’energia in un simile regime. Gli strumenti utilizzati e l’esperienza acquisita in questa tesi saranno fondamentali per questo scopo.

Measurement of the inclusive and differential t/t cross sections at 13 TeV in the all-jets boosted regime with CMS

The t/t production cross section is measured with the CMS detector in the all-jets channel in $pp$ collisions at the centre-of-mass energy of 13 TeV. The analysis is based on the study of t/t events in the boosted topology, namely events in which decay products of the quark top have a high Lorentz boost and are thus reconstructed in the detector as a single, wide jet. The data sample used in this analysis corresponds to an integrated luminosity of 2.53 fb-1. The inclusive cross section is found to be sigma(t/t) = 727 +- 46 (stat.) +115-112 (sys.) +- 20~(lumi.) pb, a value which is consistent with the theoretical predictions. The differential, detector-level cross section is measured as a function of the transverse momentum of the leading jet and compared to the QCD theoretical predictions. Finally, the differential, parton-level cross section is reported, measured as a function of the transverse momentum of the leading parton, extrapolated to the full phase space and compared to the QCD predictions.

Dynamics of Bora wind over the Adriatic sea: atmospheric water balance and role of air-sea fluxes and orography

The Bora wind is a mesoscale phenomenon which typically affects the Adriatic Sea basin for several days each year, especially during winter. The Bora wind has been studied for its intense outbreak across the Dinaric Alps. The properties of the Bora wind are widely discussed in the literature and scientific papers usually focus on the eastern Adriatic coast where strong turbulence and severe gust intensity are more pronounced. However, the impact of the Bora wind can be significant also over Italy, not only in terms of wind speed instensity. Depending on the synoptic pressure pattern (cyclonic or anticyclonic Bora) and on the season, heavy snowfall, severe storms, storm surges and floods can occur along the Adriatic coast and on the windward flanks of the Apennines. In the present work five Bora cases that occurred in recent years have been selected and their evolution has been simulated with the BOLAM-MOLOCH model set, developed at ISAC-CNR in Bologna. Each case study has been addressed by a control run and by several sensitivity tests, performed with the purpose of better understanding the role played by air-sea latent and sensible heat fluxes. The tests show that the removal of the fluxes induces modifications in the wind approching the coast and a decrease of the total precipitation amount predicted over Italy. In order to assess the role of heat fluxes, further analysis has been carried out: column integrated water vapour fluxes have been computed along the Italian coastline and an atmospheric water balance has been evaluated inside a box volume over the Adriatic Sea. The balance computation shows that, although latent heat flux produces a significant impact on the precipitation field, its contribution to the balance is relatively minor. The most significant and lasting case study, that of February 2012, has been studied in more detail in order to explain the impressive drop in the total precipitation amount simulated in the sensitivity tests with removed heat fluxes with respect to the CNTRL run. In these experiments relative humidity and potential temperature distribution over different cross-sections have been examined. With respect to the CNTRL run a drier and more stable boundary layer, characterised by a more pronounced wind shear at the lower levels, has been observed to establish above the Adriatic Sea. Finally, in order to demonstrate that also the interaction of the Bora flow with the Apennines plays a crucial role, sensitivity tests varying the orography height have been considered. The results of such sensitivity tests indicate that the propagation of the Bora wind over the Adriatic Sea, and in turn its meteorological impact over Italy, is influenced by both the large air-sea heat fluxes and the interaction with the Apennines that decelerate the upstream flow.