Time to digital converter

In questa tesi è analizzato il caso di sensori con uscita in frequenza e periodo, si traduce in ultima analisi nella capacità di misurare con precisione un intervallo temporale. La rivelazione del tempo risulta essere lo stadio fondamentale da cui deriva la risoluzione dell'intero sistema di misura. Nella realtà, la questione della simultaneità cioè individuare con assoluta precisione due eventi che si verificano contemporaneamente, in un determinato istante t, è un problema piuttosto complesso: le difficoltà sono correlate soprattutto alle limitazioni fisiche intrinseche degli strumenti di misura. E' utile allora fornire un'analisi sui principi e le tecniche alla base della misura di intervalli temporali, detta Time Interval Measurement (TIM). Lo scopo della tesi è studiare i vari metodi per realizzare TDC lineari digitali, facendo un'analisi critica e ed evidenziando pro e contro che i vari approcci presentano, attingendo e analizzando criticamente informazioni dalle varie fonti riportate in bibliografia.

Sea level trends in the Mediterranean from tide gauges and satellite altimetry

Sea level variation is one of the parameters directly related to climate change. Monitoring sea level rise is an important scientific issue since many populated areas of the world and megacities are located in low-lying regions. At present, sea level is measured by means of two techniques: the tide gauges and the satellite radar altimetry. Tide gauges measure sea-level relatively to a ground benchmark, hence, their measurements are directly affected by vertical ground motions. Satellite radar altimetry measures sea-level relative to a geocentric reference and are not affected by vertical land motions. In this study, the linear relative sea level trends of 35 tide gauge stations distributed across the Mediterranean Sea have been computed over the period 1993-2014. In order to extract the real sea-level variation, the vertical land motion has been estimated using the observations of available GPS stations and removed from the tide gauges records. These GPS-corrected trends have then been compared with satellite altimetry measurements over the same time interval (AVISO data set). A further comparison has been performed, over the period 1993-2013, using the CCI satellite altimetry data set which has been generated using an updated modeling. The absolute sea level trends obtained from satellite altimetry and GPS-corrected tide gauge data are mostly consistent, meaning that GPS data have provided reliable corrections for most of the sites. The trend values range between +2.5 and +4 mm/yr almost everywhere in the Mediterranean area, the largest trends were found in the Northern Adriatic Sea and in the Aegean. These results are in agreement with estimates of the global mean sea level rise over the last two decades. Where GPS data were not available, information on the vertical land motion deduced from the differences between absolute and relative trends are in agreement with the results of other studies.