Journal cover Journal topic
Ocean Science An interactive open-access journal of the European Geosciences Union
Journal topic

Journal metrics

IF value: 2.864
IF2.864
IF 5-year value: 3.337
IF 5-year
3.337
CiteScore value: 4.5
CiteScore
4.5
SNIP value: 1.259
SNIP1.259
IPP value: 3.07
IPP3.07
SJR value: 1.326
SJR1.326
Scimago H <br class='widget-line-break'>index value: 52
Scimago H
index
52
h5-index value: 30
h5-index30
Preprints
https://doi.org/10.5194/os-2020-46
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/os-2020-46
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

  02 Jul 2020

02 Jul 2020

Review status
This preprint is currently under review for the journal OS.

Evidence of coastal trapped wave scattering using high-frequency radar data in the Mid-Atlantic Bight

Kelsey Brunner and Kamazima M. M. Lwiza Kelsey Brunner and Kamazima M. M. Lwiza
  • Stony Brook University, School of Marine and Atmospheric Sciences, Stony Brook University, Stony Brook, New York, USA

Abstract. Coastal trapped waves (CTWs) become scattered when they encounter irregular coastlines and bathymetry during propagation. Analytical and modeling studies have provided some information about the different types of shelf geometries that can induce scattering, but much of the CTW scattering process generally remains a large knowledge gap. Furthermore, CTW scattering has never before been directly identified with observations. High-frequency radar surface velocity data covering the Mid-Atlantic Bight (MAB) continental shelf provides unprecedented observations of CTWs within a region with a highly complex coastline and bathymetry. A combination of velocity vector maps from real vector empirical orthogonal function (R-EOF) analysis and phase maps from complex empirical orthogonal function (C-EOF) analysis allow the identification of CTW scattering by assuming each EOF mode corresponds to a CTW mode. Abrupt jumps in phase in association with magnitude amplification/reduction or directional rotation of velocity vectors are indications of scattering. Using these guidelines, Georges Bank, Hudson Shelf Valley, Delaware Bay mouth, Chesapeake Bay mouth, and the North Carolina shelf are identified as high scattering regions within the MAB. Furthermore, stratification is confirmed to increase scattering into progressively higher order modes through a cascading process by comparing winter and summer cases, which supports previous theoretical and numerical model predictions. The simple methodology used here can be applied to observations of CTWs on other coastlines around the world to identify additional scattering regions and help close the knowledge gap.

Kelsey Brunner and Kamazima M. M. Lwiza

Interactive discussion

Status: final response (author comments only)
Status: final response (author comments only)
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
[Login for Authors/Topic Editors] [Subscribe to comment alert] Printer-friendly Version - Printer-friendly version Supplement - Supplement

Kelsey Brunner and Kamazima M. M. Lwiza

Kelsey Brunner and Kamazima M. M. Lwiza

Viewed

Total article views: 259 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
156 69 34 259 32 39
  • HTML: 156
  • PDF: 69
  • XML: 34
  • Total: 259
  • BibTeX: 32
  • EndNote: 39
Views and downloads (calculated since 02 Jul 2020)
Cumulative views and downloads (calculated since 02 Jul 2020)

Viewed (geographical distribution)

Total article views: 172 (including HTML, PDF, and XML) Thereof 171 with geography defined and 1 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Saved

No saved metrics found.

Discussed

No discussed metrics found.
Latest update: 19 Oct 2020
Publications Copernicus
Download
Short summary
Coastal trapped waves (CTWs) are very long shallow water waves that propagate along the continental shelves of most major ocean basins. Their general properties are known but can be easily modified by changes in the coastline or other factors through a process known as scattering. Scattering is not well understood but can cause high surface velocities. For the first time, we directly observe CTW scattering using a simple mathematical technique that can be easily applied to other coastlines.
Coastal trapped waves (CTWs) are very long shallow water waves that propagate along the...
Citation