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Quantification of Stokes drift as a ...

Clark, Matthew.

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Quantification of Stokes drift as a mechanism for surface oil advection in the Gulf of Mexico during the Deepwater Horizon oil spill.

紀錄類型:	書目-電子資源 : Monograph/item
正題名/作者:	Quantification of Stokes drift as a mechanism for surface oil advection in the Gulf of Mexico during the Deepwater Horizon oil spill./
作者:	Clark, Matthew.
面頁冊數:	35 p.
附註:	Source: Masters Abstracts International, Volume: 55-02.
Contained By:	Masters Abstracts International55-02(E).
標題:	Physical oceanography. -
電子資源:	http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=1600033
ISBN:	9781339076478

Quantification of Stokes drift as a mechanism for surface oil advection in the Gulf of Mexico during the Deepwater Horizon oil spill.
Clark, Matthew.

Quantification of Stokes drift as a mechanism for surface oil advection in the Gulf of Mexico during the Deepwater Horizon oil spill. - 35 p.

Source: Masters Abstracts International, Volume: 55-02.

Thesis (M.S.)--The Florida State University, 2015.

Wave-driven transport, also known as Stokes drift, is the motion of a particle due to the orbital motion induced by a passing wave. This orbital motion does not form closed loops, leading to a net displacement over a single wave period. Stokes drift has previously been qualitatively shown to be a factor in ocean surface particle transport, with most studies focused exclusively in near-shore regions. However, Stokes drift has never been quantified beyond theoretical studies and case studies limited to small regions. Here, Stokes drift is calculated directly from Wavewatch III model data in the Gulf of Mexico for April-July 2010. Its magnitudes are compared between deep and shelf water areas, and against the magnitudes of surface currents and parameterized wind drift. These comparisons are also made specifically for the time period surrounding the passage of Hurricane Alex through the southwestern Gulf of Mexico. While there is not a major difference between the absolute magnitudes of Stokes drift in shelf vs. deep water areas or when compared to wind drift, Stokes drift is larger in shelf water areas relative to surface currents than in deep water. During Hurricane Alex, Stokes drift magnitudes were much larger in the immediate area of the storm, while in the oil spill area there was little change until after the storm was out of the Gulf, at which time swell had propagated into the region, increasing Stokes drift magnitudes.

ISBN: 9781339076478Subjects--Topical Terms:

3168433
Physical oceanography.

Quantification of Stokes drift as a mechanism for surface oil advection in the Gulf of Mexico during the Deepwater Horizon oil spill.
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500 $a Advisers: Mark Bourassa; Eric Chassignet.
502 $a Thesis (M.S.)--The Florida State University, 2015.
520 $a Wave-driven transport, also known as Stokes drift, is the motion of a particle due to the orbital motion induced by a passing wave. This orbital motion does not form closed loops, leading to a net displacement over a single wave period. Stokes drift has previously been qualitatively shown to be a factor in ocean surface particle transport, with most studies focused exclusively in near-shore regions. However, Stokes drift has never been quantified beyond theoretical studies and case studies limited to small regions. Here, Stokes drift is calculated directly from Wavewatch III model data in the Gulf of Mexico for April-July 2010. Its magnitudes are compared between deep and shelf water areas, and against the magnitudes of surface currents and parameterized wind drift. These comparisons are also made specifically for the time period surrounding the passage of Hurricane Alex through the southwestern Gulf of Mexico. While there is not a major difference between the absolute magnitudes of Stokes drift in shelf vs. deep water areas or when compared to wind drift, Stokes drift is larger in shelf water areas relative to surface currents than in deep water. During Hurricane Alex, Stokes drift magnitudes were much larger in the immediate area of the storm, while in the oil spill area there was little change until after the storm was out of the Gulf, at which time swell had propagated into the region, increasing Stokes drift magnitudes.
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