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Author: Samantha Rachel Terker Publisher: ISBN: Category : Internal waves Languages : en Pages : 120
Book Description
The Monterey Bay region, with bathymetric features including Monterey Submarine Canyon and Sur Platform, has been a site for examination of generation, propagation and dissipation of the internal tide. Observations of propagation of the internal tide on the California continental margin and in Monterey Submarine Canyon are presented. Additionally, the development and sea-trials of the EM-POGO, a free-falling absolute velocity profiler which can be used to study the internal tide is detailed. EM-POGO: The EM-POGO is a low-cost and accurate velocity profiler. Electromagnetic current instrumentation has been added to Bathy Systems, Inc. POGO transport sondes to produce the EM-POGO. Velocity determined from measurements of motionally-induced electric fields generated by ocean currents moving through the vertical component of the Earth's magnetic field are added to the transport provided by the POGO. A refurbished EM-POGO collected 15 profiles; relative and absolute velocity uncertainty was & sim 1 cm s−1 and 0.5 - 5 cm s−1, respectively, with 25-m vertical resolution. Internal tide: North of Sur Platform but south of Monterey Submarine Canyon, a short-duration survey and a multi-week timeseries measured northward energy flux in the mean, supporting model results indicating that topographic features off Point Sur generate strong internal tides observed in the canyon. Though dominated by low modes with O(100 km) horizontal wavelengths, semidiurnal energy fluxes, kinetic and potential energies show lateral variability on O(5 km) scales. Spatial variability results, in part, from interference patterns and the sharp delineation of beams with limited azimuthal extent. A simple two-source model of a first-mode interference pattern reproduces the most striking aspects of the observations. In Monterey Submarine Canyon energy fluxes are steered by canyon bathymetry and are consistent with a numerical model. Vertical profiles reveal predominantly along-canyon flux intensified in the bottom 500 m. A rough one-dimensional along-canyon energy budget based on energy-flux divergence, dissipation rates and barotropic-to-baroclinic energy conversion rates is constructed. Cross-canyon- integrated along-canyon flux decreases from 13 ± 3.4 MW at the deepest section (1500 m) to 5.6 ± 0.3 MW at the shallowest (900 m). The largest drops (~ 7 MW and ~ 4 MW) are around meanders. The one-dimensional flux budget is, on average, balanced.
Author: Samantha Rachel Terker Publisher: ISBN: Category : Internal waves Languages : en Pages : 120
Book Description
The Monterey Bay region, with bathymetric features including Monterey Submarine Canyon and Sur Platform, has been a site for examination of generation, propagation and dissipation of the internal tide. Observations of propagation of the internal tide on the California continental margin and in Monterey Submarine Canyon are presented. Additionally, the development and sea-trials of the EM-POGO, a free-falling absolute velocity profiler which can be used to study the internal tide is detailed. EM-POGO: The EM-POGO is a low-cost and accurate velocity profiler. Electromagnetic current instrumentation has been added to Bathy Systems, Inc. POGO transport sondes to produce the EM-POGO. Velocity determined from measurements of motionally-induced electric fields generated by ocean currents moving through the vertical component of the Earth's magnetic field are added to the transport provided by the POGO. A refurbished EM-POGO collected 15 profiles; relative and absolute velocity uncertainty was & sim 1 cm s−1 and 0.5 - 5 cm s−1, respectively, with 25-m vertical resolution. Internal tide: North of Sur Platform but south of Monterey Submarine Canyon, a short-duration survey and a multi-week timeseries measured northward energy flux in the mean, supporting model results indicating that topographic features off Point Sur generate strong internal tides observed in the canyon. Though dominated by low modes with O(100 km) horizontal wavelengths, semidiurnal energy fluxes, kinetic and potential energies show lateral variability on O(5 km) scales. Spatial variability results, in part, from interference patterns and the sharp delineation of beams with limited azimuthal extent. A simple two-source model of a first-mode interference pattern reproduces the most striking aspects of the observations. In Monterey Submarine Canyon energy fluxes are steered by canyon bathymetry and are consistent with a numerical model. Vertical profiles reveal predominantly along-canyon flux intensified in the bottom 500 m. A rough one-dimensional along-canyon energy budget based on energy-flux divergence, dissipation rates and barotropic-to-baroclinic energy conversion rates is constructed. Cross-canyon- integrated along-canyon flux decreases from 13 ± 3.4 MW at the deepest section (1500 m) to 5.6 ± 0.3 MW at the shallowest (900 m). The largest drops (~ 7 MW and ~ 4 MW) are around meanders. The one-dimensional flux budget is, on average, balanced.
Author: Eugene G. Morozov Publisher: Springer ISBN: 3319731599 Category : Science Languages : en Pages : 317
Book Description
This book presents a detailed study of the structure and variability of internal tides and their geographical distribution in the ocean. Based on experimental analysis of oceanic measurements combined with numerical modeling, it offers a comprehensive overview of the internal wave processes around the globe. In particular, it is based on moored buoys observations in many regions in all oceans (Atlantic, Pacific, Indian, Arctic, and Southern) that have been carried out by researchers from different countries for more than 40 years as part of various oceanographic programs, including WOCE and CLIVAR. However, a significant portion of the data was collected by the author, who is a field oceanographer. The data was processed and interpreted on the basis of the latest knowledge of internal wave motion. The properties of internal waves were analyzed in relation to the bottom topography and mean state of the ocean in specific regions. Internal waves play a major role in the formation of seawater stratification and are responsible for the main processes of ocean dynamics, such as energy transfer and mixing. One of the most significant ideas presented in this book is the generation of internal tides over submarine ridges. Energy fluxes from submarine ridges related to tidal internal waves greatly exceed the fluxes from continental slopes. Submarine ridges form an obstacle to the propagation of tidal currents, which can cause the creation of large amplitude internal tides. Energy fluxes from submarine ridges account for approximately one fourth of the total energy dissipation of the barotropic tides. Model simulations and moored measurements have been combined to generate a map of global distribution of internal tide amplitudes. This book is of interest to oceanographers, marine biologists, civil engineers, and scientists working in climate research, fluid mechanics, acoustics, and underwater navigation.
Author: Emil T. Petruncio Publisher: ISBN: Category : Tidal currents Languages : en Pages : 124
Book Description
A first order description of tidal heights and currents in Monterey Bay is provided. Analysis of sea level records indicate that a mixed, predominantly semidiurnal tide nearly co-oscillates within the bay. Analysis of month-long moored ADCP records obtained in the winter and summer of 1992 reveals that tidal-band currents account for approximately 50 percent of the total current variance in the upper ocean (20-200 m). A relatively strong (7 cm/s) fortnightly tide (MSf) is present in both seasons. Considerable rotation of the semidiurnal ellipse orientations occurs with depth during both seasons. A month- long record of surface current measurements obtained with CODAR, an HF radar system, during September 1992 reveals that the Monterey Submarine Canyon clearly influences the strength and direction of semidiurnal (M2) tidal currents. Good agreement exists between the strength and orientation of ADCP- and CODAR-derived tidal ellipses, with the exception of the constituent K1. Large, spatially uniform K1 surface currents (20-30 cm/s) appear to be the result of diurnal sea breeze forcing.
Author: Publisher: ISBN: Category : Bores (Tidal phenomena) Languages : en Pages : 76
Book Description
Internal tidal bore events observed at a Monterey Bay inner shelf site are analyzed. A six month data set from the Naval Postgraduate School Monterey Inner Shelf Observatory site included water column current velocities and thermal structure data. Isothermal displacements paired with concurrent velocity observations in the water column were used to assess the events' individual characteristics as the internal tidal bores shoal and approach the surf zone. The primary hypothesis tested was that if the internal tidal bores observed at MISO had strong along-shore current velocity signatures, then those bores were most likely generated at the Monterey Bay Submarine Canyon edge or were evidence of an internal edge wave. If velocity signatures were primarily cross-shore, then bores would most likely propagate from straight across the shelf westward from their generation site at the continental shelf break. Visual observations of temperature profiles, current vector plots, linear regressions, and histograms were employed to test the relationships between forcing, stratification, and internal tidal bore forms. The unique aspect of this research is the focus on shoaling effects of internal tidal bores after they have traversed the continental shelf and impinge on the nearshore. Additionally, coastlines with significant bathymetric features, like Monterey Bay, are of operational interest to the military and are prime generation sites for these internal bore and soliton events. Internal tidal bores can directly impact naval special operations; specifically, amphibious landings and SEAL Delivery Vehicle operations. Understanding where and how bore and soliton events are generated is beneficial to nearshore modelers and operators.
Author: Emil T. Petruncio Publisher: ISBN: Category : Science Languages : en Pages : 210
Book Description
Shipboard ADCP and CTD measurements were conducted in Monterey Submarine Canyon in April and October 1994 to determine the propagation characteristics and energy levels of the semidiurnal internal tide. The measurements reveal a bottom intensified internal tide propagating energy up canyon. The region of strongest motion is in a beam 150-200 m thick, centered approximately 150 m above the Canyon floor. Along canyon baroclinic M2 currents are typically 15-20 cm/s, an order of magnitude larger than the estimated barotropic tidal currents. In April 1994, the internal tidal beam is well described by a progressive wave, while in October 1994, the signal is standing along and perpendicular to the beam. The Princeton Ocean Model was used to study the generation and propagation of semidiurnal internal tides in submarine canyons and to investigate their sensitivity to canyon shape.
Author: Kim A. Koehler Publisher: ISBN: Category : Ocean currents Languages : en Pages : 132
Book Description
April and May of 1988 along the central California coast were characterized as a period of strong coastal upwelling produced by moderate to strong northwesterly winds present throughout the period. A product of this upwelling event was the manifestation of southward geostrophic currents which extended to a distance of approximately 50 km from the coast. From 08 to 11 May 1988, hydrographic surveying was conducted within the Monterey Bay. Internal waves, with amplitudes of up to 30 m were present throughout the period and effectively masked the mean signal, implying that averaging is essential to avoid aliasing. The current -- temperature -- depth (CTD) data were averaged to estimate the mean field during this time frame. Acoustic Doppler Current Profiler (ADCP) data, were also averaged. The mean flow field and dynamic topography implied anticyclonic surface flow with cyclonic flow at 200 m depth. ADCP derived mean flows compared favorably with geostrophic mean flow rate in all areas except one, the deep outflow region along the northern wall of the Canyon. Application of ocean models of boundary layer flow of the geostrophic mean field yielded flows similar to those described above. Wind stress experiments indicated that strong wind field may influence surface circulation in the Bay. Interactions between the coastal upwelling geostrophic jet and the Monterey Submarine Canyon is believed to have been a major mechanism responsible for the mean flow.
Author: Steven Michael Jachec Publisher: ISBN: 9780549060482 Category : Languages : en Pages : 276
Book Description
Traditionally, it has been viewed that tides dissipate 2.6 TW over the continental shelves via the shallow bottom boundary layer, and have little impact on deep ocean mixing (Munk & Wunsch, 1998). Through their tidal maps, Egbert & Ray (2001) have confirmed that while most energy is lost in the shallow sea, nearly 1 TW is lost in the deep ocean (Garrett, 2003). Internal tides may provide the mechanism to bring power to mix the deep ocean (Garrett, 2003). However, the exact amounts dissipated in the shallow coastal regional and deep ocean remain in question.
Author: Paul O'Connor Publisher: ISBN: Category : Monterey Bay (Calif.) Languages : en Pages : 140
Book Description
A method was devised by which short-term deviations from the astronomical tides at Monterey, California were detected and measured in the absence of the predicted tides at Monterey. This was accomplished by comparing the observed tides at Monterey with the predicted tides at San Francisco. The sealevel deviations, or anomalies, that can be found using this method range in duration from several hours to two or three days. The sea-level variations that were detected during a six-month period at Monterey had magnitudes ranging between +0.9 and -0.8 of a foot and durations ranging from 3.5 to 39.5 hours. The largest anomalies found are attributed to sea breezes that were unaccompanied by any appreciable atmospheric pressure variations. On the other hand, pressure changes accompanying frontal passages appear to be the dominant cause of other anomalies in spite of wind effects. Time lags in the response of sea level to weather phenomena were as long as three hours. (Author).
Author: William W. Broenkow Publisher: ISBN: Category : Monterey Bay (Calif.) Languages : en Pages : 52
Book Description
During a 25-hour hydrographic times series at two stations near the head of Monterey Submarine Canyon, an internal tide was observed with an amplitude of 80 to 115 m in water depths of 120 and 220 m respectively. These large oscillations produced daily variations in hydrographic and chemical parameters that were of the same magnitude as seasonal variations in Monterey Bay. Computed velocities associated with the internal tide were on the order of 10 em/sec, and this tidally induced circulation may have a significant role in the exchange of deep water between Monterey Submarine Canyon and the open ocean.
Author: Samantha Rachel Terker
Author: Samantha Rachel Terker
Author: Eugene G. Morozov
Author: Emil T. Petruncio
Author: 
Author: Emil T. Petruncio
Author: Kim A. Koehler
Author: Steven Michael Jachec
Author: Paul O'Connor
Author: William W. Broenkow
Author: