The Experts below are selected from a list of 453 Experts worldwide ranked by ideXlab platform

Kwok Fai Cheung - One of the best experts on this subject based on the ideXlab platform.

  • adcp observations of edge waves off oahu in the wake of the november 2006 kuril islands tsunami
    Geophysical Research Letters, 2007
    Co-Authors: Jeremy D Bricker, Sophie Munger, Christine Pequignet, Judith R Wells, Geno Pawlak, Kwok Fai Cheung
    Abstract:

    Received 13 September 2007; revised 5 October 2007; accepted 8 November 2007; published 15 December 2007. [1] During the 2006 Kuril Islands tsunami, edge waves propagating along Oahu’s south shore were observed via depth-averaged ADCP Velocity and pressure data acquired in real-time by a coastal observatory at 12 m depth and 400 m offshore. Time-varying rotary-Component Velocity spectra obtained via wavelet analysis agree with the phase lag observed between pressure and each Cartesian Velocity Component, in indicating the directions of rotation and travel of progressive edge waves. Furthermore, the theoretical ratios between power in the free surface elevation and in each Velocity Component of edge waves, agree with those observed, and a nonlinear shallow-water model shows edge waves of various modes propagating along the shore near our observation location. Importantly, the maximum surge in sea level occurred at a time when edge waves of all constituent frequencies were superposed. Citation: Bricker, J. D., S. Munger, C. Pequignet, J. R. Wells, G. Pawlak, and K. F. Cheung (2007), ADCP observations of edge waves off Oahu in the wake of the November 2006 Kuril Islands tsunami, Geophys. Res. Lett., 34, L23617, doi:10.1029/ 2007GL032015.

Jeremy D Bricker - One of the best experts on this subject based on the ideXlab platform.

  • adcp observations of edge waves off oahu in the wake of the november 2006 kuril islands tsunami
    Geophysical Research Letters, 2007
    Co-Authors: Jeremy D Bricker, Sophie Munger, Christine Pequignet, Judith R Wells, Geno Pawlak, Kwok Fai Cheung
    Abstract:

    Received 13 September 2007; revised 5 October 2007; accepted 8 November 2007; published 15 December 2007. [1] During the 2006 Kuril Islands tsunami, edge waves propagating along Oahu’s south shore were observed via depth-averaged ADCP Velocity and pressure data acquired in real-time by a coastal observatory at 12 m depth and 400 m offshore. Time-varying rotary-Component Velocity spectra obtained via wavelet analysis agree with the phase lag observed between pressure and each Cartesian Velocity Component, in indicating the directions of rotation and travel of progressive edge waves. Furthermore, the theoretical ratios between power in the free surface elevation and in each Velocity Component of edge waves, agree with those observed, and a nonlinear shallow-water model shows edge waves of various modes propagating along the shore near our observation location. Importantly, the maximum surge in sea level occurred at a time when edge waves of all constituent frequencies were superposed. Citation: Bricker, J. D., S. Munger, C. Pequignet, J. R. Wells, G. Pawlak, and K. F. Cheung (2007), ADCP observations of edge waves off Oahu in the wake of the November 2006 Kuril Islands tsunami, Geophys. Res. Lett., 34, L23617, doi:10.1029/ 2007GL032015.

Sophie Munger - One of the best experts on this subject based on the ideXlab platform.

  • adcp observations of edge waves off oahu in the wake of the november 2006 kuril islands tsunami
    Geophysical Research Letters, 2007
    Co-Authors: Jeremy D Bricker, Sophie Munger, Christine Pequignet, Judith R Wells, Geno Pawlak, Kwok Fai Cheung
    Abstract:

    Received 13 September 2007; revised 5 October 2007; accepted 8 November 2007; published 15 December 2007. [1] During the 2006 Kuril Islands tsunami, edge waves propagating along Oahu’s south shore were observed via depth-averaged ADCP Velocity and pressure data acquired in real-time by a coastal observatory at 12 m depth and 400 m offshore. Time-varying rotary-Component Velocity spectra obtained via wavelet analysis agree with the phase lag observed between pressure and each Cartesian Velocity Component, in indicating the directions of rotation and travel of progressive edge waves. Furthermore, the theoretical ratios between power in the free surface elevation and in each Velocity Component of edge waves, agree with those observed, and a nonlinear shallow-water model shows edge waves of various modes propagating along the shore near our observation location. Importantly, the maximum surge in sea level occurred at a time when edge waves of all constituent frequencies were superposed. Citation: Bricker, J. D., S. Munger, C. Pequignet, J. R. Wells, G. Pawlak, and K. F. Cheung (2007), ADCP observations of edge waves off Oahu in the wake of the November 2006 Kuril Islands tsunami, Geophys. Res. Lett., 34, L23617, doi:10.1029/ 2007GL032015.

Christine Pequignet - One of the best experts on this subject based on the ideXlab platform.

  • adcp observations of edge waves off oahu in the wake of the november 2006 kuril islands tsunami
    Geophysical Research Letters, 2007
    Co-Authors: Jeremy D Bricker, Sophie Munger, Christine Pequignet, Judith R Wells, Geno Pawlak, Kwok Fai Cheung
    Abstract:

    Received 13 September 2007; revised 5 October 2007; accepted 8 November 2007; published 15 December 2007. [1] During the 2006 Kuril Islands tsunami, edge waves propagating along Oahu’s south shore were observed via depth-averaged ADCP Velocity and pressure data acquired in real-time by a coastal observatory at 12 m depth and 400 m offshore. Time-varying rotary-Component Velocity spectra obtained via wavelet analysis agree with the phase lag observed between pressure and each Cartesian Velocity Component, in indicating the directions of rotation and travel of progressive edge waves. Furthermore, the theoretical ratios between power in the free surface elevation and in each Velocity Component of edge waves, agree with those observed, and a nonlinear shallow-water model shows edge waves of various modes propagating along the shore near our observation location. Importantly, the maximum surge in sea level occurred at a time when edge waves of all constituent frequencies were superposed. Citation: Bricker, J. D., S. Munger, C. Pequignet, J. R. Wells, G. Pawlak, and K. F. Cheung (2007), ADCP observations of edge waves off Oahu in the wake of the November 2006 Kuril Islands tsunami, Geophys. Res. Lett., 34, L23617, doi:10.1029/ 2007GL032015.

Judith R Wells - One of the best experts on this subject based on the ideXlab platform.

  • adcp observations of edge waves off oahu in the wake of the november 2006 kuril islands tsunami
    Geophysical Research Letters, 2007
    Co-Authors: Jeremy D Bricker, Sophie Munger, Christine Pequignet, Judith R Wells, Geno Pawlak, Kwok Fai Cheung
    Abstract:

    Received 13 September 2007; revised 5 October 2007; accepted 8 November 2007; published 15 December 2007. [1] During the 2006 Kuril Islands tsunami, edge waves propagating along Oahu’s south shore were observed via depth-averaged ADCP Velocity and pressure data acquired in real-time by a coastal observatory at 12 m depth and 400 m offshore. Time-varying rotary-Component Velocity spectra obtained via wavelet analysis agree with the phase lag observed between pressure and each Cartesian Velocity Component, in indicating the directions of rotation and travel of progressive edge waves. Furthermore, the theoretical ratios between power in the free surface elevation and in each Velocity Component of edge waves, agree with those observed, and a nonlinear shallow-water model shows edge waves of various modes propagating along the shore near our observation location. Importantly, the maximum surge in sea level occurred at a time when edge waves of all constituent frequencies were superposed. Citation: Bricker, J. D., S. Munger, C. Pequignet, J. R. Wells, G. Pawlak, and K. F. Cheung (2007), ADCP observations of edge waves off Oahu in the wake of the November 2006 Kuril Islands tsunami, Geophys. Res. Lett., 34, L23617, doi:10.1029/ 2007GL032015.