東華大學圖書館 |

語系: 繁體中文

說明(常見問題)

回圖書館首頁

手機版館藏查詢

登入

回首頁

切換: 標籤 | MARC模式 | ISBD

Shear instability of longshore curre...

Li, Ye.

FindBook

Google Book

Amazon

博客來

Shear instability of longshore currents and their interaction with gravity waves.

紀錄類型:	書目-電子資源 : Monograph/item
正題名/作者:	Shear instability of longshore currents and their interaction with gravity waves./
作者:	Li, Ye.
面頁冊數:	96 p.
附註:	Source: Dissertation Abstracts International, Volume: 65-02, Section: B, page: 0968.
Contained By:	Dissertation Abstracts International65-02B.
標題:	Engineering, Marine and Ocean. -
電子資源:	http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=3121986

Shear instability of longshore currents and their interaction with gravity waves.
Li, Ye.

Shear instability of longshore currents and their interaction with gravity waves. - 96 p.

Source: Dissertation Abstracts International, Volume: 65-02, Section: B, page: 0968.

Thesis (Ph.D.)--University of Michigan, 2004.

When wind-generated gravity waves propagate towards the shoreline with an oblique incidence angle, they shoal and break in the surf zone, generating longshore currents. These currents are generally unstable and large amplitude shear waves are excited. Since wave-driven currents in the nearshore region greatly affect sediment transport, a good understanding of the wave-induced nearshore circulation system is important to accurately predict the transport of sediments. The dynamics of nearshore processes is also of scientific interest because various time and length scale motions coexist and they interact. Here the generation and evolution of low-frequency shear waves and their interaction with high-frequency incoming gravity waves are studied both analytically and numerically. Linear stability analyses for various longshore current profiles are carried out, and special attention is paid to the free surface effect. It is found that the free surface reduces both the linear growth rate and the unstable wave number. Dynamics of unstable longshore currents beyond the linear regime is studied by solving the shallow water equations numerically. Small disturbances grow into large amplitude shear waves and large-scale coherent vortices (eddies) are often formed. In order to shed light on the process of the formation of eddies, simple mathematical models are derived using systematic asymptotic expansion. Compared with full numerical simulations of the shallow water equations, numerical solutions of the new asymptotic models are shown to correctly capture the process of wave steepening, which eventually leads the waves to break. In order to better predict the nearshore circulation system, wave-current interaction is included and numerical simulations of the coupled shallow water and wave action equations are carried out. Our results show that this interaction process significantly changes the dynamics of wave-induced nearshore circulation.Subjects--Topical Terms:

1019064
Engineering, Marine and Ocean.

Shear instability of longshore currents and their interaction with gravity waves.
LDR:02841nmm 2200277 4500 001 1861511
005 20041117064928.5
008 130614s2004 eng d
035 $a (UnM)AAI3121986
035 $a AAI3121986
040 $a UnM $c UnM
100 1 $a Li, Ye. $3 1949106
245 1 0 $a Shear instability of longshore currents and their interaction with gravity waves.
300 $a 96 p.
500 $a Source: Dissertation Abstracts International, Volume: 65-02, Section: B, page: 0968.
500 $a Chairman: Wooyoung Choi.
502 $a Thesis (Ph.D.)--University of Michigan, 2004.
520 $a When wind-generated gravity waves propagate towards the shoreline with an oblique incidence angle, they shoal and break in the surf zone, generating longshore currents. These currents are generally unstable and large amplitude shear waves are excited. Since wave-driven currents in the nearshore region greatly affect sediment transport, a good understanding of the wave-induced nearshore circulation system is important to accurately predict the transport of sediments. The dynamics of nearshore processes is also of scientific interest because various time and length scale motions coexist and they interact. Here the generation and evolution of low-frequency shear waves and their interaction with high-frequency incoming gravity waves are studied both analytically and numerically. Linear stability analyses for various longshore current profiles are carried out, and special attention is paid to the free surface effect. It is found that the free surface reduces both the linear growth rate and the unstable wave number. Dynamics of unstable longshore currents beyond the linear regime is studied by solving the shallow water equations numerically. Small disturbances grow into large amplitude shear waves and large-scale coherent vortices (eddies) are often formed. In order to shed light on the process of the formation of eddies, simple mathematical models are derived using systematic asymptotic expansion. Compared with full numerical simulations of the shallow water equations, numerical solutions of the new asymptotic models are shown to correctly capture the process of wave steepening, which eventually leads the waves to break. In order to better predict the nearshore circulation system, wave-current interaction is included and numerical simulations of the coupled shallow water and wave action equations are carried out. Our results show that this interaction process significantly changes the dynamics of wave-induced nearshore circulation.
590 $a School code: 0127.
650 4 $a Engineering, Marine and Ocean. $3 1019064
650 4 $a Geophysics. $3 535228
650 4 $a Physical Oceanography. $3 1019163
690 $a 0547
690 $a 0373
690 $a 0415
710 2 0 $a University of Michigan. $3 777416
773 0 $t Dissertation Abstracts International $g 65-02B.
790 1 0 $a Choi, Wooyoung, $e advisor
790 $a 0127
791 $a Ph.D.
792 $a 2004
856 4 0 $u http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=3121986