Thesis (M. Sc.)--Carleton University, 1990. / Also available in electronic format on the Internet.

Thesis (M. Phil.)--University of Hong Kong, 2005. / Title proper from title frame. Also available in printed format.

Many astronomical observations, including rotational curve measurements of stars and the analysis of the cosmic microwave background, suggest the existence of an invisible matter density content in the Universe, commonly called Dark Matter (DM). Possibly, DM could be of particle nature, where Weakly Interacting Massive Particles (WIMPs) could be a viable DM candidate. The cubic-kilometer sized IceCube neutrino observatory located at the Earth’s South Pole can search indirectly for the existence of DM by detecting neutrino signals from WIMP self-annihilation in the Galactic center (GC) and the Galactic halo (GH). Two main physics analyses were developed and conducted to search indirectly for WIMP self-annihilation in the Milky Way’s GC and GH. Signal hypotheses for different WIMP annihilation channels, WIMP masses and DM halo profiles were tested. The results of both analyses were compatible with the background-only hypothesis for all tested signal hypotheses. Thus, upper limits at the 90% confidence level (C.L.) on the thermally averaged DM self-annihilation cross-section, &lt;σΑv&gt;, were set. Dedicated atmospheric muon veto techniques have been developed for the GC search making such an IceCube analysis possible for the first time. The GC analysis utilized data from 319.7 days of live-time of the IceCube detector running in its 79-string configuration during 2010 and 2011, whereas the GH analysis utilized pre-existing data samples developed for point-like neutrino sources with a live-time of 1701.9 days between 2008 and 2013. The most stringent upper limits on &lt;σΑv&gt; were obtained for WIMP annihilation directly into a pair of neutrinos assuming a Navarro-Frenk-White (NFW) DM halo profile. Conducting the GC and GH analyses for this annihilation channel an upper limit on &lt;σΑv&gt; as low as 4.0 · 10-24 cm3 s-1 and 4.5 · 10-24 cm3 s-1 is set for a 65 GeV and 500 GeV massive WIMP, respectively. These galactic indirect neutrino searches for DM are complementary to the indirect gamma-ray DM searches usually performed on extra-galactic targets like spheroidal dwarf galaxies. / <p>At the time of the doctoral defense, the following paper was unpublished and had a status as follows: Paper 2: Manuscript.</p>

Thesis (M.A.) - Carleton University, 2003. / Includes bibliographical references (p. 219-224). Also available in electronic format on the Internet.

Thesis (M.Sc.) - Carleton University, 2005. / Includes bibliographical references (p. 138-141). Also available in electronic format on the Internet.

Thesis (M.Sc.) - Carleton University, 2005. / Includes bibliographical references (p. 66). Also available in electronic format on the Internet.

Thesis (M.Sc.) - Carleton University, 2005. / Includes bibliographical references (p. 125-130). Also available in electronic format on the Internet.

Thesis (M. Sc.)--Carleton University, 1996. / Also available in electronic format on the Internet.

The Radio Neutrino Observatory in Greenland (RNO-G) is a multidisciplinary, multinational collaboration which uses antennas to detect neutrino interactions with arctic ice sheets. Neutrinos are formed from nuclear reactions; predominant sources include nuclear reactors, stars, supernovae, and the big bang. They rarely interact with normal matter and thus travel from origin to destination relatively unimpeded, with applications including tracking nuclear weapons tests and supernovae. Measurements of galactic neutrino flux can provide information about how the universe developed and its current evolution. Neutrino interactions produce signals from 100 to 1000MHz. Current RNO-G antennas operate over only a portion of this band; 200MHz for horizontally polarized (Hpol) and 400MHz for vertically polarized (Vpol). In this thesis, multiple lengths of Hpol antennas are combined, and exponentially tapered geometry is added to the Vpol antenna to improve performance. Both polarizations are combined into one structure to improve observatory performance. This thesis details the design, fabrication, and testing of a new RNO-G antenna iteration. Each design is compared to frequency, gain, matching, and size requirements. Two variations of the final design are fabricated and tested, with performance compared to simulation.

Das IceCube Neutrinoteleskop hat im Jahr 2013 erstmals einen isotropen, quasi-diffusen astrophysikalischen Neutrinoflusses detektiert. Dieser Fluss kann jedoch bisher keiner astrophysikalischen Quellklasse zugeordnet werden. Um nach kurzlebigen Neutrinoquellen zu suchen, wurde 2008 das optische und Röntgen-Nachfolgebeobachtungsprogramm des IceCube Detektors eingerichtet. Es sucht nach zwei oder mehr Neutrinoereignissen, die von einer Punkquelle stammen könnten und innerhalb von 100s detektiert werden. Ein solches Signal wird unter anderem von langen oder kurzen Gammastrahlungsblitzen (GRBs) erwartet oder von verwandten Objekten wie leuchtschwachen GRBs oder Supernovae mit relativistischen Jets. Die Alarmraten des Nachfolgebeobachtungsprogramms sind jedoch niedrig und bieten bisher keine Hinweise für die Existenz von kurzlebigen Neutrinoquellen. Das Nachfolgebeobachungsprogramm hat bisher nur ein einziges Neutrinotriplet detektiert, das der Auslöser für eine umfassende Beobachtungskampagne war. In den optischen, Röntgen- und Gammastrahlungsbeobachtungen wurde keine wahrscheinliche Neutrinoquelle identifiziert und eine Supernova oder ein heller GRB können ausgeschlossen werden. Das Neutrinotriplet kann entweder eine zufällige Koinzidenz von Untergrundereignissen sein (alle 13.7 Jahre erwartet) oder es kann von einer leuchtschwachen oder besonders schnell verblassenden Quelle stammen. Die niedrige Rate von Neutrinomultipletts stellt außerdem eine obere Schranke auf die Helligkeit von kurzlebigen Neutrinoquellen dar. Seltene Quellen mit lokalen Raten von < 3e-8 – 10e-5 Mpc^-3 Jahr^-1 können nicht den gesammten Fluss erzeugen, ohne die detektierte Anzahl Multipletts zu überschreiten. Der Fluss von GRBs ist dadurch auf 5-30% des astrophysikalischen Flusses beschränkt. Falls 1% aller Kernkollaps-Supernovae einen Jet besitzen, der auf die Erde zeigt, so können sie 40-100% des Flusses erzeugen und ihre durchschnittliche Neutrinohelligkeit ist <3e51erg. / The IceCube neutrino observatory first detected and isotropic, quasi-diffuse astrophysical neutrino flux in 2013. However, this flux can so far not be associated with an astrophysical source class. To search for short-lived neutrino sources, the optical and X-ray follow-up program was established in 2008. It searches for two or more neutrino events that might origin from a point source and are detected within 100s. Such a signal is expected from long or short gamma-ray bursts (GRBs) or from related objects like low-luminosity GRBs or supernovae with choked jets. The alert rates of the follow-up program are however low, such that they do not provide evidence for the existence of short-lived neutrino sources. So far the follow-up program has only detected a one neutrino triplet, which triggered an extensive follow-up campaign. No likely neutrino source was detected in the collected optical, X-ray and gamma-ray observations and the presence of a supernova or a bright GRB can be excluded. The neutrino triplet can either be a chance coincidence of background events (expected every 13.7 years) or is can originate from a faint or quickly fading astrophysical source. The low rate of neutrino multiplets moreover provides an upper limit on the luminosity of short-lived neutrino sources. Rare sources with local rates of < 3e-8 – 10e-5 Mpc^-3 yr^-1 cannot produce the complete fluc without producing too many neutrino multiplets. This limits the contribution of GRBs to 5-30% of the astrophysical flux. If 1% of all core-collapse supernovae have a jet that is pointed at Earth, they can emit up to 40-100% of the flux and their average neutrino luminosity is <3e51erg.