Internal Waves on the Continental Shelf of the Northwestern Arabian Gulf

Turbulent fluxes and mixing due to internal waves (IWs) play a major role in transporting nutrients, affecting biological productivity and water-borne constituents such as contaminants and sediments. To better understand IWs on the continental shelf of the northwestern Arabian Gulf, off the coast of...

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Main Authors: Fahad Al Senafi, Ayal Anis
Format: Article
Language:English
Published: Frontiers Media S.A. 2020-01-01
Series:Frontiers in Marine Science
Subjects:
Online Access:https://www.frontiersin.org/article/10.3389/fmars.2019.00805/full
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spelling doaj-3f88ab863f794243ab35877e2eee33622020-11-25T02:04:00ZengFrontiers Media S.A.Frontiers in Marine Science2296-77452020-01-01610.3389/fmars.2019.00805509056Internal Waves on the Continental Shelf of the Northwestern Arabian GulfFahad Al Senafi0Ayal Anis1Department of Marine Science, College of Science, Kuwait University, Kuwait City, KuwaitDepartment of Oceanography, Texas A&M University, College Station, TX, United StatesTurbulent fluxes and mixing due to internal waves (IWs) play a major role in transporting nutrients, affecting biological productivity and water-borne constituents such as contaminants and sediments. To better understand IWs on the continental shelf of the northwestern Arabian Gulf, off the coast of Kuwait, we conducted a study to examine the characteristics of these waves, and the associated energy cascade from IWs to turbulence. The study was conducted during midsummer (15 to 27 July, 2017), collected spatial transects and time series measurements at five moorings. Continuous turbulence profiles were taken at four locations in the vicinity of the moorings. Measurements of temperature, salinity, currents, turbidity, chlorophyll a, and turbulence reveal that IW activity was consistent with the diurnal and semidiurnal tidal cycles. Based on cross shore tracking of the IWs, it was estimated that the IWs propagated toward the coast at an average speed of 0.31 m/s. IW amplitudes ranged from 7 to 9 m and were observed to generate intense mixing (>10−7 W/kg). In addition, we examined nighttime convective conditions driven by surface buoyancy flux which were estimated to contribute up to 70% of the turbulence kinetic energy (TKE) production. The results presented here shed new light on IW characteristics in the Northern Arabian Gulf, and offer the first detailed study of these waves in this region.https://www.frontiersin.org/article/10.3389/fmars.2019.00805/fullArabian (Persian) Gulfinternal wavesinternal tidesKuwaitturbulence
collection DOAJ
language English
format Article
sources DOAJ
author Fahad Al Senafi
Ayal Anis
spellingShingle Fahad Al Senafi
Ayal Anis
Internal Waves on the Continental Shelf of the Northwestern Arabian Gulf
Frontiers in Marine Science
Arabian (Persian) Gulf
internal waves
internal tides
Kuwait
turbulence
author_facet Fahad Al Senafi
Ayal Anis
author_sort Fahad Al Senafi
title Internal Waves on the Continental Shelf of the Northwestern Arabian Gulf
title_short Internal Waves on the Continental Shelf of the Northwestern Arabian Gulf
title_full Internal Waves on the Continental Shelf of the Northwestern Arabian Gulf
title_fullStr Internal Waves on the Continental Shelf of the Northwestern Arabian Gulf
title_full_unstemmed Internal Waves on the Continental Shelf of the Northwestern Arabian Gulf
title_sort internal waves on the continental shelf of the northwestern arabian gulf
publisher Frontiers Media S.A.
series Frontiers in Marine Science
issn 2296-7745
publishDate 2020-01-01
description Turbulent fluxes and mixing due to internal waves (IWs) play a major role in transporting nutrients, affecting biological productivity and water-borne constituents such as contaminants and sediments. To better understand IWs on the continental shelf of the northwestern Arabian Gulf, off the coast of Kuwait, we conducted a study to examine the characteristics of these waves, and the associated energy cascade from IWs to turbulence. The study was conducted during midsummer (15 to 27 July, 2017), collected spatial transects and time series measurements at five moorings. Continuous turbulence profiles were taken at four locations in the vicinity of the moorings. Measurements of temperature, salinity, currents, turbidity, chlorophyll a, and turbulence reveal that IW activity was consistent with the diurnal and semidiurnal tidal cycles. Based on cross shore tracking of the IWs, it was estimated that the IWs propagated toward the coast at an average speed of 0.31 m/s. IW amplitudes ranged from 7 to 9 m and were observed to generate intense mixing (>10−7 W/kg). In addition, we examined nighttime convective conditions driven by surface buoyancy flux which were estimated to contribute up to 70% of the turbulence kinetic energy (TKE) production. The results presented here shed new light on IW characteristics in the Northern Arabian Gulf, and offer the first detailed study of these waves in this region.
topic Arabian (Persian) Gulf
internal waves
internal tides
Kuwait
turbulence
url https://www.frontiersin.org/article/10.3389/fmars.2019.00805/full
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