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Journal articles on the topic 'Coastal Trapped Waves'

Author: Grafiati

Published: 4 June 2021

Last updated: 21 February 2023

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1

Haines, John W., Keith R. Thompson, and Doug P. Wiens. "The detection of coastal-trapped waves." Journal of Geophysical Research: Oceans 96, no. C2 (1991): 2593–97. http://dx.doi.org/10.1029/90jc02218.

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2

Johnson, E. R., and J. T. Rodney. "Spectral methods for coastal-trapped waves." Continental Shelf Research 31, no. 14 (2011): 1481–89. http://dx.doi.org/10.1016/j.csr.2011.06.009.

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3

Musgrave, R. C. "Energy Fluxes in Coastal Trapped Waves." Journal of Physical Oceanography 49, no. 12 (2019): 3061–68. http://dx.doi.org/10.1175/jpo-d-18-0172.1.

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AbstractThe calculation of energy flux in coastal trapped wave modes is reviewed in the context of tidal energy pathways near the coast. The significant barotropic pressures and currents associated with coastal trapped wave modes mean that large errors in estimating the wave flux are incurred if only the baroclinic component is considered. A specific example is given showing that baroclinic flux constitutes only 10% of the flux in a mode-1 wave for a reasonable choice of stratification and bathymetry. The interpretation of baroclinic energy flux and barotropic-to-baroclinic conversion at the c

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4

Middleton, John F., and Daniel G. Wright. "Coastal-trapped waves on the Labrador Shelf." Journal of Geophysical Research: Oceans 96, no. C2 (1991): 2599–617. http://dx.doi.org/10.1029/90jc02129.

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5

Brink, K. H. "Coastal-trapped waves with finite bottom friction." Dynamics of Atmospheres and Oceans 41, no. 3-4 (2006): 172–90. http://dx.doi.org/10.1016/j.dynatmoce.2006.05.001.

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6

Jordi, A., A. Orfila, G. Basterretxea, and J. Tintoré. "Coastal trapped waves in the northwestern Mediterranean." Continental Shelf Research 25, no. 2 (2005): 185–96. http://dx.doi.org/10.1016/j.csr.2004.09.012.

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7

Freeland, H. J., F. M. Boland, J. A. Church, et al. "The Australian Coastal Experiment: A Search for Coastal-Trapped Waves." Journal of Physical Oceanography 16, no. 7 (1986): 1230–49. http://dx.doi.org/10.1175/1520-0485(1986)016<1230:taceas>2.0.co;2.

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8

Brink, K. H. "On the Damping of Free Coastal-Trapped Waves." Journal of Physical Oceanography 20, no. 8 (1990): 1219–25. http://dx.doi.org/10.1175/1520-0485(1990)020<1219:otdofc>2.0.co;2.

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9

Dale, Andrew C., John M. Huthnance, and Toby J. Sherwin. "Coastal-Trapped Waves and Tides at Near-Inertial Frequencies." Journal of Physical Oceanography 31, no. 10 (2001): 2958–70. http://dx.doi.org/10.1175/1520-0485(2001)031<2958:ctwata>2.0.co;2.

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10

Mitsudera, Humio, and Kimio Hanawa. "Frictional coastal trapped waves in a two-layered ocean." Journal of Fluid Mechanics 198, no. -1 (1989): 453. http://dx.doi.org/10.1017/s0022112089000212.

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11

Morrow, R. A., Ian S. F. Jones, R. L. Smith, and P. J. Stabeno. "Bass Strait Forcing of Coastal Trapped Waves: ACE Revisited." Journal of Physical Oceanography 20, no. 9 (1990): 1528–38. http://dx.doi.org/10.1175/1520-0485(1990)020<1528:bsfoct>2.0.co;2.

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12

Clarke, Allan J. "Origin of the Coastally Trapped Waves Observed during the Australian Coastal Experiment." Journal of Physical Oceanography 17, no. 11 (1987): 1847–59. http://dx.doi.org/10.1175/1520-0485(1987)017<1847:ootctw>2.0.co;2.

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13

REZNIK, G. M., and V. ZEITLIN. "Resonant excitation of trapped waves by Poincaré waves in the coastal waveguides." Journal of Fluid Mechanics 673 (February 24, 2011): 349–94. http://dx.doi.org/10.1017/s0022112010006300.

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After having revisited the theory of linear waves in the rotating shallow-water model with a straight coast and arbitrary shelf/beach bathymetry, we undertake a detailed study of resonant interaction of free Poincaré waves with modes trapped in the coastal waveguide. We describe and quantify the mechanisms of resonant excitation of waveguide modes and their subsequent nonlinear saturation. We obtain the modulation equations for the amplitudes of excited waveguide modes in the absence and in the presence of spatial modulation and analyse their solutions. Different saturation regimes are exhibit

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14

Ray, Sthitapragya, Debadatta Swain, Meer M. Ali, and Mark A. Bourassa. "Coastal Upwelling in the Western Bay of Bengal: Role of Local and Remote Windstress." Remote Sensing 14, no. 19 (2022): 4703. http://dx.doi.org/10.3390/rs14194703.

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Monsoon winds drive upwelling along the eastern coast of India. This study examined the role of coastally trapped Kelvin waves in modulating the seasonal variability of local alongshore windstress (AWS)-driven coastal upwelling along the western Bay of Bengal. The winds generated AWS resulting in a positive cross-shore Ekman transport (ET) from March to the end of September, which forced coastal upwelling along the eastern coast of India. However, coastally trapped Kelvin waves could also modulate this process by raising or lowering the thermocline. Remotely sensed windstress, sea surface temp

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15

Nuss, Wendell A. "Synoptic-Scale Structure and the Character of Coastally Trapped Wind Reversals." Monthly Weather Review 135, no. 1 (2007): 60–81. http://dx.doi.org/10.1175/mwr3267.1.

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Abstract Coastally trapped wind reversals that occur along the U.S. West Coast have been described in numerous other studies. The synoptic-scale environment and the forcing of a coastally trapped Kelvin wave are highly linked in the development of these wind reversals. However, not all wind reversals appear to behave like propagating Kelvin waves and the analysis of coastal buoy observations for three years indicates that different types of disturbances occur. Both propagating disturbances and nonpropagating disturbances occur with similar frequencies. While the synoptic-scale characteristics

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16

Cahill, Madeleine L., Jason H. Middleton, and Basil R. Stanton. "Coastal-Trapped Waves on the West Coast of South Island, New Zealand." Journal of Physical Oceanography 21, no. 4 (1991): 541–57. http://dx.doi.org/10.1175/1520-0485(1991)021<0541:ctwotw>2.0.co;2.

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17

Weaver, AJ. "Bass Strait as a reverse estuary source for coastally trapped waves." Marine and Freshwater Research 38, no. 6 (1987): 685. http://dx.doi.org/10.1071/mf9870685.

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The water in Bass Strait is often denser than the surrounding Tasman Sea water, especially in winter. This phenomenon is modelled numerically as a Rossby adjustment problem. Coastally trapped waves are generated when dense Bass Strait water flows over deepening bottom topography, through the joint effect of baroclinicity and relief (JEBAR). A narrow northward flowing stream is also observed at the shelf edge. These results are compared with field observations and the Austraian Coastal Experiment. The flow at the eastern mouth of Bass Strait is also described briefly.

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18

LAMB, KEVIN G. "Shoaling solitary internal waves: on a criterion for the formation of waves with trapped cores." Journal of Fluid Mechanics 478 (March 10, 2003): 81–100. http://dx.doi.org/10.1017/s0022112002003269.

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Shoaling solitary internal waves are ubiquitous features in the coastal regions of the world's oceans where waves with a core of recirculating fluid (trapped cores) can provide an effective transport mechanism. Here, numerical evidence is presented which suggests that there is a close connection between the limiting behaviour of large-amplitude solitary waves and the formation of such waves via shoaling. For some background states, large-amplitude waves are broad, having a nearly horizontal flow in their centre. The flow in the centre of such waves is called a conjugate flow. For other backgro

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19

de Freitas, Pedro Paulo, Afonso de Moraes Paiva, Mauro Cirano, et al. "Coastal trapped waves propagation along the Southwestern Atlantic Continental Shelf." Continental Shelf Research 226 (September 2021): 104496. http://dx.doi.org/10.1016/j.csr.2021.104496.

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20

Middleton, John F., and Mark A. Merrifield. "The Scattering of Long Coastal-Trapped Waves in Frictional Seas." Journal of Physical Oceanography 25, no. 4 (1995): 502–12. http://dx.doi.org/10.1175/1520-0485(1995)025<0502:tsolct>2.0.co;2.

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21

Brink, K. H. "Scattering of long coastal-trapped waves due to bottom irregularities." Dynamics of Atmospheres and Oceans 10, no. 2 (1986): 149–64. http://dx.doi.org/10.1016/0377-0265(86)90004-7.

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22

Wallace, H. M., and A. J. Willmott. "Coastal-trapped waves in elliptical lakes and around elliptical islands." Geophysical & Astrophysical Fluid Dynamics 56, no. 1-4 (1991): 81–114. http://dx.doi.org/10.1080/03091929108219513.

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23

Rodney, J. T., and E. R. Johnson. "Meanders and Eddies from Topographic Transformation of Coastal-Trapped Waves." Journal of Physical Oceanography 44, no. 4 (2014): 1133–50. http://dx.doi.org/10.1175/jpo-d-12-0224.1.

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Abstract This paper describes how topographic variations can transform a small-amplitude, linear, coastal-trapped wave (CTW) into a nonlinear wave or an eddy train. The dispersion relation for CTWs depends on the slope of the shelf. Provided the cross-shelf slope varies sufficiently slowly along the shelf, the local structure of the CTW adapts to the local geometry and the wave transformation can be analyzed by the Wentzel–Kramers–Brillouin–Jeffreys (WKBJ) method. Two regions of parameter space are straightforward: adiabatic transmission (where, at the incident wave frequency, a long wave exis

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24

Connolly, Thomas P., Barbara M. Hickey, Igor Shulman, and Richard E. Thomson. "Coastal Trapped Waves, Alongshore Pressure Gradients, and the California Undercurrent*." Journal of Physical Oceanography 44, no. 1 (2014): 319–42. http://dx.doi.org/10.1175/jpo-d-13-095.1.

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Abstract The California Undercurrent (CUC), a poleward-flowing feature over the continental slope, is a key transport pathway along the west coast of North America and an important component of regional upwelling dynamics. This study examines the poleward undercurrent and alongshore pressure gradients in the northern California Current System (CCS), where local wind stress forcing is relatively weak. The dynamics of the undercurrent are compared in the primitive equation Navy Coastal Ocean Model and a linear coastal trapped wave model. Both models are validated using hydrographic data and curr

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25

Freeland, Howard J. "Diurnal Coastal-Trapped Waves on the East Australian Continental Shelf." Journal of Physical Oceanography 18, no. 4 (1988): 690–94. http://dx.doi.org/10.1175/1520-0485(1988)018<0690:dctwot>2.0.co;2.

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26

Maiwa, Kazuyuki, Yukio Masumoto, and Toshio Yamagata. "Characteristics of coastal trapped waves along the southern and eastern coasts of Australia." Journal of Oceanography 66, no. 2 (2010): 243–58. http://dx.doi.org/10.1007/s10872-010-0022-z.

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27

Forbes, AMG. "Wind stress in the Australian coastal experiment region." Marine and Freshwater Research 38, no. 4 (1987): 475. http://dx.doi.org/10.1071/mf9870475.

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During the 6 months of the Australian Coastal Experiment (ACE), recordings were made by the Australian Bureau of Meteorology of several meteorological parameters at a number of coastal stations and by the CSIRO at several offshore locations to complement the ACE current-meter and sea-level gauge array. The aim was to examine the wind field over the New South Wales coast and so determine the magnitude of long shelf wind stress, which might locally force coastal trapped waves (CTW). Wind stress decreased equatorward, with the greatest potential for local CTW forcing lying on the southernmost con

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28

Yin, Liping, Fangli Qiao, and Quanan Zheng. "Coastal-Trapped Waves in the East China Sea Observed by a Mooring Array in Winter 2006." Journal of Physical Oceanography 44, no. 2 (2014): 576–90. http://dx.doi.org/10.1175/jpo-d-13-07.1.

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Abstract Using five mooring array observations in the coastal water of the East China Sea (ECS) in winter 2006, the authors identify three kinds of low-frequency waves using the ensemble empirical mode decomposition (EEMD) method. The analysis indicates that the periods of the waves varied from 2 to 10 days, which are consistent with coastal-trapped wave (CTW) modes: the Kelvin wave (KW) mode, the first shelf wave (SW1) mode, and the second shelf wave (SW2) mode. An analytical model is established and the dispersion relation of the waves from the analytical method agrees well with the observat

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29

Church, John A., and Howard J. Freeland. "The Energy Source for the Coastal-Trapped Waves in the Australian Coastal Experiment Region." Journal of Physical Oceanography 17, no. 3 (1987): 289–300. http://dx.doi.org/10.1175/1520-0485(1987)017<0289:tesftc>2.0.co;2.

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30

Aydın, Müjdat, and Şükrü Turan Beşiktepe. "Mechanism of generation and propagation characteristics of coastal trapped waves in the Black Sea." Ocean Science 18, no. 4 (2022): 1081–91. http://dx.doi.org/10.5194/os-18-1081-2022.

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Abstract. Coastal trapped waves (CTW) are a major mechanism to distribute energy from the atmosphere in the ocean and play a significant role in large-scale, low-frequency sea-level and current variability in continental shelf and slope areas. Despite their significance for coastal dynamics, observational evidence of the influence of CTWs on the large-scale circulation is rather limited. In this study, mode-1 coastal trapped waves that were captured at sea-level stations at five locations along the southern coast of the Black Sea are examined together with sea surface height reanalysis from th

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31

Louis, JP. "Current-Shelf interactions during the Australian Coastal experiment." Marine and Freshwater Research 40, no. 5 (1989): 571. http://dx.doi.org/10.1071/mf9890571.

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Current-meter records from the Australian Coastal Experiment are examined. In addition to the long, coastal-trapped waves with λ > 800 km that this experiment was specifically designed to investigate, the current records also show distinct event-like bursts of wave activity. These events appear to be related to offshore current structures and are observed over the slope as low-frequency current oscillations with periods of 3-5 days and lasting for 3-4 cycles. It is postulated that these topographic waves are generated by the interaction of the East Australian Current and associated eddies w

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32

Taylor, Andy, and Gary B. Brassington. "Sea Level Anomaly Forecasts on a Coastal Waveguide." Weather and Forecasting 35, no. 2 (2020): 757–70. http://dx.doi.org/10.1175/waf-d-18-0198.1.

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Abstract An approach to reduce forecast data to coastal waveguide coordinates is described and demonstrated, informed by the literature on coastally trapped waves (CTWs). All discussion is limited to the Australian mainland but the approach is generally relevant to regions where CTWs influence sea level, including the Americas and Africa. The approach does not produce new forecasts, but aims to focus forecaster attention on aspects of sea level forecasts prominent on the long Australian coast. The approach also explicitly addresses spatial issues associated with measuring coastal paths. Coasta

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33

Rodney, J. T., and E. R. Johnson. "Localisation of coastal trapped waves by longshore variations in bottom topography." Continental Shelf Research 32 (January 2012): 130–37. http://dx.doi.org/10.1016/j.csr.2011.11.002.

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34

Brink, K. H. "Coastal-Trapped Waves and Wind-Driven Currents Over the Continental Shelf." Annual Review of Fluid Mechanics 23, no. 1 (1991): 389–412. http://dx.doi.org/10.1146/annurev.fl.23.010191.002133.

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35

Liao, Fanglou, and Xiao Hua Wang. "A Numerical Study of Coastal-Trapped Waves in Jervis Bay, Australia." Journal of Physical Oceanography 48, no. 11 (2018): 2555–69. http://dx.doi.org/10.1175/jpo-d-18-0106.1.

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AbstractCoastal-trapped waves (CTWs) in Jervis Bay were investigated using a Jervis Bay Ocean Model (JBOM), based on the Princeton Ocean Model. Under the typical temperature stratification in Jervis Bay in summer, the first three modes of external CTWs can scatter into the bay. The wind stress inside Jervis Bay can generate CTWs, and the wind stress on the adjacent shelf can also generate CTWs in the bay by oscillations at the bay's opening, which are associated with temperature fluctuations there. The actual subinertial CTWs in Jervis Bay are a result of the interference of these CTWs. The am

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36

Wilkin, John L., and David C. Chapman. "Scattering of Coastal-Trapped Waves by Irregularities in Coastline and Topography." Journal of Physical Oceanography 20, no. 3 (1990): 396–421. http://dx.doi.org/10.1175/1520-0485(1990)020<0396:soctwb>2.0.co;2.

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37

Schumann, E. H., and K. H. Brink. "Coastal-Trapped Waves off the Coast of South Africa: Generation, Propagation and Current Structures." Journal of Physical Oceanography 20, no. 8 (1990): 1206–18. http://dx.doi.org/10.1175/1520-0485(1990)020<1206:ctwotc>2.0.co;2.

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38

Ma, Hong. "Trapped internal gravity waves in a geostrophic boundary current." Journal of Fluid Mechanics 247 (February 1993): 205–29. http://dx.doi.org/10.1017/s0022112093000448.

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The effect of a geostrophic boundary current on internal gravity waves is studied with a reduced-gravity model. We found that the boundary current not only modifies the coastal Kelvin wave, but also forms wave guides for short internal gravity waves. The combined effects of current shear, the boundary, and the slope of the interface create the trapping mechanism. These trapped internal gravity waves appear as groups of discrete zonal modes. They have wavelengths comparable to or shorter than the internal Rossby radius of deformation. Their phase speeds are close to that of the internal Kelvin

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39

Sansón, L. Zavala. "Simple Models of Coastal-Trapped Waves Based on the Shape of the Bottom Topography." Journal of Physical Oceanography 42, no. 3 (2012): 420–29. http://dx.doi.org/10.1175/jpo-d-11-053.1.

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Abstract Solutions of barotropic coastal-trapped waves in the shallow-water context are discussed for different shapes of the bottom topography. In particular, an infinite family of topographic waves over continental shelves characterized by a shape parameter is considered. The fluid depth is proportional to xs, where x is the offshore coordinate and s is a real, positive number. The model assumes the rigid-lid approximation and a semi-infinite domain 0 ≤ x ≤ ∞. The wave structure and the dispersion relation depend explicitly on the shape parameter s. Essentially, waves over steeper shelves po

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40

Igeta, Yosuke, Yujiro Kitade, and Masaji Matsuyama. "Numerical Experiments on Scattering of Coastal-Trapped Waves by Topography and Bays." Oceanography in Japan 14, no. 3 (2005): 441–58. http://dx.doi.org/10.5928/kaiyou.14.441.

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41

Pizarro, Oscar, and Gary Shaffer. "Wind-Driven, Coastal-Trapped Waves off the Island of Gotland, Baltic Sea." Journal of Physical Oceanography 28, no. 11 (1998): 2117–29. http://dx.doi.org/10.1175/1520-0485(1998)028<2117:wdctwo>2.0.co;2.

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42

Reynaud, Thierry, R. Grant Ingram, Howard J. Freeland, and Andrew J. Weaver. "Propagation of coastal‐trapped waves under an ice cover in Hudson Bay*." Atmosphere-Ocean 30, no. 4 (1992): 593–620. http://dx.doi.org/10.1080/07055900.1992.9649457.

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43

Schlosser, Tamara L., Nicole L. Jones, Ruth C. Musgrave, Cynthia E. Bluteau, Gregory N. Ivey, and Andrew J. Lucas. "Observations of Diurnal Coastal-Trapped Waves with a Thermocline-Intensified Velocity Field." Journal of Physical Oceanography 49, no. 7 (2019): 1973–94. http://dx.doi.org/10.1175/jpo-d-18-0194.1.

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AbstractUsing 18 days of field observations, we investigate the diurnal (D1) frequency wave dynamics on the Tasmanian eastern continental shelf. At this latitude, the D1 frequency is subinertial and separable from the highly energetic near-inertial motion. We use a linear coastal-trapped wave (CTW) solution with the observed background current, stratification, and shelf bathymetry to determine the modal structure of the first three resonant CTWs. We associate the observed D1 velocity with a superimposed mode-zero and mode-one CTW, with mode one dominating mode zero. Both the observed and mode-

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44

Inall, Mark E., Frank Nilsen, Finlo R. Cottier, and Ragnhild Daae. "Shelf/fjord exchange driven by coastal‐trapped waves in the A rctic." Journal of Geophysical Research: Oceans 120, no. 12 (2015): 8283–303. http://dx.doi.org/10.1002/2015jc011277.

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45

Flores-Vidal, X., R. Durazo, L. Zavala-Sansón, et al. "Evidence of inertially generated coastal-trapped waves in the eastern tropical Pacific." Journal of Geophysical Research: Oceans 119, no. 5 (2014): 3121–33. http://dx.doi.org/10.1002/2013jc009118.

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46

Stepanov, D. V., and V. V. Novotryasov. "Sub-inertial modulation of nonlinear Kelvin waves in the coastal zone." Nonlinear Processes in Geophysics 20, no. 3 (2013): 357–64. http://dx.doi.org/10.5194/npg-20-357-2013.

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Abstract. Observational evidence is presented for interaction between nonlinear internal Kelvin waves at the ωt,i (where the ωt is the semidiurnal frequency and the ωi is the inertial frequency) and random oscillations of the background coastal current at the sub-inertial Ω frequency in the Japan/East Sea. Enhanced coastal currents at the sum ω+ and difference ω-frequencies ω±=ωt,i ± Ω have properties of propagating Kelvin waves, which suggests permanent energy exchange from the sub-inertial band to the mesoscale ω± band. This interaction may be responsible for a greater-than-predicted intensi

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47

Davies, Alan M., and Jiuxing Xing. "The Effect of a Bottom Shelf Front upon the Generation and Propagation of Near-Inertial Internal Waves in the Coastal Ocean." Journal of Physical Oceanography 35, no. 6 (2005): 976–90. http://dx.doi.org/10.1175/jpo2732.1.

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Abstract A three-dimensional nonlinear baroclinic model in cross-sectional form is used to study the generation and propagation of wind-forced near-inertial internal waves in a coastal region in the presence of a bottom front. Initially calculations are performed with the front in an infinite domain region. By this means coastal effects are removed. The initial response is in terms of inertial oscillations in the surface layer. However, in the frontal area these are modified by interaction through the nonlinear momentum terms with regions of positive and negative vorticity associated with the

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48

Jiang, Lin, Changming Dong, and Liping Yin. "Cross-shelf transport induced by coastal trapped waves along the coast of East China Sea." Journal of Oceanology and Limnology 36, no. 3 (2018): 630–40. http://dx.doi.org/10.1007/s00343-018-7008-x.

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49

Igeta, Yosuke, Yujiro Kitade, and Masaji Matsuyama. "Characteristics of coastal-trapped waves induced by typhoon along the southeast coast of Honshu, Japan." Journal of Oceanography 63, no. 5 (2007): 745–60. http://dx.doi.org/10.1007/s10872-007-0064-z.

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50

Yuan, Dongliang. "Dynamics of the Cold-Water Event off the Southeast Coast of the United States in the Summer of 2003." Journal of Physical Oceanography 36, no. 10 (2006): 1912–27. http://dx.doi.org/10.1175/jpo2950.1.

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Abstract The cold-water event along the southeast coast of the United States in the summer of 2003 is studied using satellite data combined with in situ observations. The analysis suggests that the cooling is produced by wind-driven coastal upwelling, which breaks the thermocline barrier in the summer of 2003. The strong and persistent southwesterly winds in the summer of 2003 play an important role of lifting the bottom isotherms up to the surface and away from the coast, generating persistent surface cooling in July–August 2003. Once the thermocline barrier is broken, the stratification in t

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