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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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 |
work_keys_str_mv |
AT fahadalsenafi internalwavesonthecontinentalshelfofthenorthwesternarabiangulf AT ayalanis internalwavesonthecontinentalshelfofthenorthwesternarabiangulf |
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