Thèse de doctorat--Sciences naturelles--Faculté des sciences de Paris, 1888. N°: 638.

Thesis (doctoral)--K. technische Hochschule zu München, 1903. / Bibliography: p. 117.

Resonant water waves in closed or semi-closed fluid systems are referred to as "seiches". Literature on this topic in recent years can be found in this thesis. This research is based on wave data in three coastal bays at the southern coast of Vancouver Island opening to Juan de Fuca Strait. Preliminary aim is to look for the nature and cause of the observed wave motions of these bays. Time series analysis and numerical modeling are performed to reveal seiche nature and develop a method to predict frequency response of bays with arbitrary shapes and variable depths. The method is evaluated through its application in the three coastal bays. Results of spectral analysis and numerical model agree well. The possible energy sources of observed seiches are discussed. Edge waves were the major source of observed seiches. The strongest seiches observed were attributed to Proudman coupling between pressure waves and water waves. Oceanic internal tides may contribute energy to a fortnightly pattern of seiche activity. / Science, Faculty of / Earth, Ocean and Atmospheric Sciences, Department of / Graduate

Thesis (Ph.D.) -- Dept. of Mathematics, University of Adelaide, 1971.

x, various paging : ill. / Title page, contents and abstract only. The complete thesis in print form is available from the University Library. / Thesis (Ph.D.)--Dept. of Mathematics, University of Adelaide, 1971

x, various paging : ill. / Title page, contents and abstract only. The complete thesis in print form is available from the University Library. / Thesis (Ph.D.)--Dept. of Mathematics, University of Adelaide, 1971

Series temporais de correntes, vento (força e direção), temperatura e salinidade, com duração de 24h, obtidas em 5 estações na Baia da Ilha Grande (rj), de 3-29/01/82, foram analisadas. As medições de corrente foram feitas a5, 12 e 20m, a cada 5min e a 2m acima do fundo, a cada 12min; temperatura e salinidade em cinco profundidades a cada 3h e vento a cada 1h. Foram utilizadas análises de series temporais através dos métodos diretos (periodograma) e indireto para as estimativas espectrais alisadas, bem como as equações hidrodinâmicas na determinação dos períodos. Foram utilizados os testes: ruído branco e fisher-whittle, a análise dos espectros rotatórios e a análise cruzada entre vento e corrente, ao longo de três camadas: superfície intermediaria e de fundo. Foram determinadas oscilações de 4,8h e identificadas como seiches internos e detectadas oscilações com período de 3,4h associadas à ressonância com o vento. Em todo o sistema da baia o período de 6h mostrou-se significativo, correspondendo à oscilação natural da baia. Foram detectadas oscilações de alta freqüência 11 e 20min, 20cm/s eventualmente associadas a vórtices e meandros da corrente. Água subtropical na camada de fundo da baia / Temporal series of currents, wind, water temperature and salinity, obtained from 5 oceanographic stations located in and around Ilha Grande Bay (RJ, Brazil), from January 23 to 29, 1982, were analyzed. AlI series have 24 hours. Currents measu¬rements were dione at depths of 5, 12, 20 m (every 5 minutes) and near the bottom (every 12 minutes). Temperature and salinity data were taken from 5 depths every 3 hours for each, while the wind was measured every hour. The present work was per¬formed in order to investigate short-period oscillations present in the region, related to density stratification and to the features of the basin, as well as to describe the circulation patterns and currents variations during one day interval. Two kinds of analysis were used: temporal series analysis, using statistical and spectral methods, and calculations by hydrodynamic motion equations. In temporal series analysis the direct (periodogram) and indirect methods were used for the spectral estimations. White-noise, Fisher- Whittle tests and rotational spectra analysis were also applied, besides the cross spectrum analysis for the data about winds and currents. The results indicate an intense and unidirectional circulation in the layer above 5 meters, from the western to the eastern portion of the Bay, through Central Channel. In this layer, on the eastern sea-opening side, a flux toward the Bay was observed. These motions, within 5 meters depth, were attributed to a circulation generated by a horizontal density difference between oceanic and inshore waters, with few contribution from tides and winds. At intermediate and near bottom layers, a horizontal homogeneity was observed and, consequent1y, smaller horizontal density gradients were detected. This way, circulation caused by tides was stronger than the movements forced by su¬perficial layers. Resultant bottom currents, observed at the Bay openings, led to the open-sea. At Central Channel, 4.8 h period oscillations were detected, and identified as internal seiches. In the eastern Portion, 3.4 hour period oscillations were detected, related to wind resonance. In alI the bay-system, the 6.0 hour period was significant, corresponding to the bay\'s natural oscillation. The study area presented a density stratification in two layers, with a single water type filling alI the portion below the 20 meters. This water, with characteristics of Subtropical Water, occupied the bottom layer due to an upwelling process produced by the dynamics of currents and winds in the continental shelf . In the two stations located off the bay, the wind and currents observations support this upwelling hypothesis.

Series temporais de correntes, vento (força e direção), temperatura e salinidade, com duração de 24h, obtidas em 5 estações na Baia da Ilha Grande (rj), de 3-29/01/82, foram analisadas. As medições de corrente foram feitas a5, 12 e 20m, a cada 5min e a 2m acima do fundo, a cada 12min; temperatura e salinidade em cinco profundidades a cada 3h e vento a cada 1h. Foram utilizadas análises de series temporais através dos métodos diretos (periodograma) e indireto para as estimativas espectrais alisadas, bem como as equações hidrodinâmicas na determinação dos períodos. Foram utilizados os testes: ruído branco e fisher-whittle, a análise dos espectros rotatórios e a análise cruzada entre vento e corrente, ao longo de três camadas: superfície intermediaria e de fundo. Foram determinadas oscilações de 4,8h e identificadas como seiches internos e detectadas oscilações com período de 3,4h associadas à ressonância com o vento. Em todo o sistema da baia o período de 6h mostrou-se significativo, correspondendo à oscilação natural da baia. Foram detectadas oscilações de alta freqüência 11 e 20min, 20cm/s eventualmente associadas a vórtices e meandros da corrente. Água subtropical na camada de fundo da baia / Temporal series of currents, wind, water temperature and salinity, obtained from 5 oceanographic stations located in and around Ilha Grande Bay (RJ, Brazil), from January 23 to 29, 1982, were analyzed. AlI series have 24 hours. Currents measu¬rements were dione at depths of 5, 12, 20 m (every 5 minutes) and near the bottom (every 12 minutes). Temperature and salinity data were taken from 5 depths every 3 hours for each, while the wind was measured every hour. The present work was per¬formed in order to investigate short-period oscillations present in the region, related to density stratification and to the features of the basin, as well as to describe the circulation patterns and currents variations during one day interval. Two kinds of analysis were used: temporal series analysis, using statistical and spectral methods, and calculations by hydrodynamic motion equations. In temporal series analysis the direct (periodogram) and indirect methods were used for the spectral estimations. White-noise, Fisher- Whittle tests and rotational spectra analysis were also applied, besides the cross spectrum analysis for the data about winds and currents. The results indicate an intense and unidirectional circulation in the layer above 5 meters, from the western to the eastern portion of the Bay, through Central Channel. In this layer, on the eastern sea-opening side, a flux toward the Bay was observed. These motions, within 5 meters depth, were attributed to a circulation generated by a horizontal density difference between oceanic and inshore waters, with few contribution from tides and winds. At intermediate and near bottom layers, a horizontal homogeneity was observed and, consequent1y, smaller horizontal density gradients were detected. This way, circulation caused by tides was stronger than the movements forced by su¬perficial layers. Resultant bottom currents, observed at the Bay openings, led to the open-sea. At Central Channel, 4.8 h period oscillations were detected, and identified as internal seiches. In the eastern Portion, 3.4 hour period oscillations were detected, related to wind resonance. In alI the bay-system, the 6.0 hour period was significant, corresponding to the bay\'s natural oscillation. The study area presented a density stratification in two layers, with a single water type filling alI the portion below the 20 meters. This water, with characteristics of Subtropical Water, occupied the bottom layer due to an upwelling process produced by the dynamics of currents and winds in the continental shelf . In the two stations located off the bay, the wind and currents observations support this upwelling hypothesis.