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  • 1
    Online Resource
    Online Resource
    American Meteorological Society ; 2022
    In:  Journal of Atmospheric and Oceanic Technology Vol. 39, No. 10 ( 2022-10), p. 1541-1559
    In: Journal of Atmospheric and Oceanic Technology, American Meteorological Society, Vol. 39, No. 10 ( 2022-10), p. 1541-1559
    Abstract: High-frequency radars (HFR) remotely measure ocean surface currents based on the Doppler shift of electromagnetic waves backscattered by surface gravity waves with one-half of the electromagnetic wavelength, called Bragg waves. Their phase velocity is affected by their interactions with the mean Eulerian currents and with all of the other waves present at the sea surface. Therefore, HFRs should measure a quantity related to the Stokes drift in addition to mean Eulerian currents. However, different expressions have been proposed for this quantity: the filtered surface Stokes drift, one-half of the surface Stokes drift, and the weighted depth-averaged Stokes drift. We evaluate these quantities using directional wave spectra measured by bottom-mounted acoustic wave and current (AWAC) profilers in the lower Saint Lawrence Estuary, Quebec, Canada, deployed in an area covered by four HFRs: two Wellen radars (WERA) and two coastal ocean dynamics applications radars (CODAR). Since HFRs measure the weighted depth-averaged Eulerian currents, we extrapolate the Eulerian currents measured by the AWACs to the sea surface assuming linear Ekman dynamics to perform the weighted depth averaging. During summer 2013, when winds are weak, correlations between the AWAC and HFR currents are stronger (0.93) than during winter 2016/17 (0.42–0.62), when winds are high. After adding the different wave-induced quantities to the Eulerian currents measured by the AWACs, however, correlations during winter 2016/17 significantly increase. Among the different expressions tested, the highest correlations (0.80–0.96) are obtained using one-half of the surface Stokes drift, suggesting that HFRs measure the latter in addition to mean Eulerian currents.
    Type of Medium: Online Resource
    ISSN: 0739-0572 , 1520-0426
    Language: Unknown
    Publisher: American Meteorological Society
    Publication Date: 2022
    detail.hit.zdb_id: 2021720-1
    detail.hit.zdb_id: 48441-6
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  • 2
    Online Resource
    Online Resource
    American Meteorological Society ; 2020
    In:  Journal of Physical Oceanography Vol. 50, No. 1 ( 2020-01), p. 197-215
    In: Journal of Physical Oceanography, American Meteorological Society, Vol. 50, No. 1 ( 2020-01), p. 197-215
    Abstract: Observations of waves, winds, turbulence, and the geometry and circulation of windrows were made in a shallow bay in the winter of 2018 outside of Rimouski, Québec. Water velocities measured from a forward-looking pulse-coherent ADCP mounted on a small zodiac show spanwise (cross-windrow) convergence, streamwise (downwind) velocity enhancement, and downwelling in the windrows, consistent with the view that windrows are the result of counterrotating pairs of wind-aligned vortices. The spacing of windrows, measured with acoustic backscatter and with surface imagery, was measured to be approximately twice the water depth, which suggests an aspect ratio of 1. The magnitude and vertical distribution of turbulence measured from the ADCP are consistent with a previous scaling and observations of near-surface turbulence under breaking waves, with dissipation rates larger and decaying faster vertically than what is expected from a shear-driven boundary layer. Measurements of dissipation rate are partitioned to within, and outside of the windrow convergence zones, and measurements inside the convergence zones are found to be nearly an order of magnitude larger than those outside with similar vertical structure. A ratio of time scales suggests that turbulence likely dissipates before it can be advected horizontally into convergences, but the advection of wave energy into convergences may elevate the surface flux of TKE and could explain the elevated turbulence in the windrows. These results add to a limited number of conflicting observations of turbulence variability due to windrows, which may modify gas flux, and heat and momentum transport in the surface boundary layer.
    Type of Medium: Online Resource
    ISSN: 0022-3670 , 1520-0485
    Language: Unknown
    Publisher: American Meteorological Society
    Publication Date: 2020
    detail.hit.zdb_id: 2042184-9
    detail.hit.zdb_id: 184162-2
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  • 3
    Online Resource
    Online Resource
    IOP Publishing ; 2014
    In:  Environmental Research Letters Vol. 9, No. 5 ( 2014-05-01), p. 054001-
    In: Environmental Research Letters, IOP Publishing, Vol. 9, No. 5 ( 2014-05-01), p. 054001-
    Type of Medium: Online Resource
    ISSN: 1748-9326
    Language: Unknown
    Publisher: IOP Publishing
    Publication Date: 2014
    detail.hit.zdb_id: 2255379-4
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  • 4
    Online Resource
    Online Resource
    Universidad Nacional Autonoma de Tayacaja Daniel Hernandez Morillo ; 2020
    In:  TAYACAJA Vol. 3, No. 2 ( 2020-11-01)
    In: TAYACAJA, Universidad Nacional Autonoma de Tayacaja Daniel Hernandez Morillo, Vol. 3, No. 2 ( 2020-11-01)
    Abstract: En el Perú existen más de 532,000 personas sordas con 23 intérpretes y un solo colegio especial donde se enseña el lenguaje de señas, aunque en el país se reconoce oficialmente la lengua de señas peruana (LSP). Esta investigación tuvo como objetivo diseñar una aplicación móvil que facilite el aprendizaje de LSP. Se probó esta aplicación móvil educativa con los estudiantes dentro y fuera del aula, con los padres de familia, y personas del entorno. La aplicación móvil facilitó a las personas con esta discapacidad a mejorar la comunicación versátil, sin necesidad de tener un intérprete a su lado.
    Type of Medium: Online Resource
    ISSN: 2617-9156
    Language: Unknown
    Publisher: Universidad Nacional Autonoma de Tayacaja Daniel Hernandez Morillo
    Publication Date: 2020
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  • 5
    Online Resource
    Online Resource
    American Meteorological Society ; 2016
    In:  Journal of Atmospheric and Oceanic Technology Vol. 33, No. 3 ( 2016-03), p. 539-550
    In: Journal of Atmospheric and Oceanic Technology, American Meteorological Society, Vol. 33, No. 3 ( 2016-03), p. 539-550
    Abstract: High-frequency radars (HFRs) measure ocean surface currents remotely through the Bragg scattering of radio waves by surface gravity waves with wavelengths shorter than 50 m. HFR range is affected by sea ice, which dampens surface gravity waves and limits wind fetch for adjacent open waters. HFR range sensitivity to sea ice concentration was empirically determined for two types of HFR—Coastal Ocean Dynamics Applications Radar (CODAR) and Wellen Radar (WERA)—installed on the shores of the lower St. Lawrence estuary, Canada, during winter 2013. One CODAR was operating at 13.5 MHz on the southern shore, and one WERA was operating at 16.15 MHz on the northern shore. Ranges were determined using a signal-to-noise ratio threshold of 6 dB for first-order Bragg scattering measured by the receive antenna elements. Ranges were normalized for expected ranges in ice-free conditions, using empirical relationships determined during summer 2013 between the range and surface gravity wave energy at the Bragg frequencies. Normalized ranges Γ decrease approximately linearly with increasing sea ice concentration C (averaged over the ice-free observational domain) with a slope close to −1 for both HFR types, that is, Γ = 1 − C. However, for a given sea ice concentration, range can vary significantly depending on the sea ice spatial distribution.
    Type of Medium: Online Resource
    ISSN: 0739-0572 , 1520-0426
    Language: Unknown
    Publisher: American Meteorological Society
    Publication Date: 2016
    detail.hit.zdb_id: 2021720-1
    detail.hit.zdb_id: 48441-6
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  • 6
    Online Resource
    Online Resource
    American Meteorological Society ; 2018
    In:  Journal of Physical Oceanography Vol. 48, No. 8 ( 2018-08), p. 1885-1901
    In: Journal of Physical Oceanography, American Meteorological Society, Vol. 48, No. 8 ( 2018-08), p. 1885-1901
    Abstract: Ocean surface wave radiation stress represents the flux of momentum due to the waves. When waves are dissipated or reflected by sea ice, that momentum is absorbed or reflected, resulting in a horizontal forcing that frequently compresses the ice. In this work, wave radiation stress is used to estimate the compressive force applied by waves to the marginal ice zone (MIZ). It is balanced by an ice internal compressive stress based on Mohr–Coulomb granular materials theory. The ice internal stress can be related to ice thickness, allowing this force balance to be used as a model for the estimation of MIZ ice thickness. The model was validated and tested using data collected during two field campaigns in the St. Lawrence estuary in 2016 and 2017. Modeled ice thickness was found to be consistent with the mean measured ice thickness over the conditions available. The range of validity of the model is discussed, and a definition of MIZ extent, based on the relative strength of wind and wave forcing, is proposed.
    Type of Medium: Online Resource
    ISSN: 0022-3670 , 1520-0485
    Language: Unknown
    Publisher: American Meteorological Society
    Publication Date: 2018
    detail.hit.zdb_id: 2042184-9
    detail.hit.zdb_id: 184162-2
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  • 7
    Online Resource
    Online Resource
    The Oceanography Society ; 2018
    In:  Oceanography Vol. 31, No. 4 ( 2018-12-01), p. 81-91
    In: Oceanography, The Oceanography Society, Vol. 31, No. 4 ( 2018-12-01), p. 81-91
    Type of Medium: Online Resource
    ISSN: 1042-8275
    Language: Unknown
    Publisher: The Oceanography Society
    Publication Date: 2018
    detail.hit.zdb_id: 1167549-4
    detail.hit.zdb_id: 2268693-9
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  • 8
    In: International Journal of Neurorehabilitation, OMICS Publishing Group, Vol. 04, No. 03 ( 2017)
    Type of Medium: Online Resource
    ISSN: 2376-0281
    Language: Unknown
    Publisher: OMICS Publishing Group
    Publication Date: 2017
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