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  1. NTU Theses and Dissertations Repository
  2. 理學院
  3. 海洋研究所
請用此 Handle URI 來引用此文件: http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/52402
完整後設資料紀錄
DC 欄位值語言
dc.contributor.advisor陳世楠(Shih-Nan Chen)
dc.contributor.authorSih-Yu Chenen
dc.contributor.author陳思妤zh_TW
dc.date.accessioned2021-06-15T16:13:51Z-
dc.date.available2016-09-25
dc.date.copyright2015-09-25
dc.date.issued2014
dc.date.submitted2015-08-18
dc.identifier.citationAllen, J. S., and P.
A. Newberger 1996 Downwelling circulation on the Oregon
continental shelf. Part I: Response to idealized
forcing. J. Phys. Oceanogr., 26, 2011–2035.
Austin, J. A., and
S. J. Lentz 2002 The inner shelf response to wind-driven
upwelling and downwelling. J. Phys.
Oceanogr., 32, 2171–2193.
Chao, S. Y. 1988 Wind-driven motion of estuarine plumes, J.
Phys. Oceanogr., 18, 1144-1166.
Chapman, D. C.,
and S. J. Lentz 1994 Trapping of a coastal density front by the
bottom boundary layer, J. Phys. Oceanogr.,
24, 1464-1478.
Chen, S. N. 2014 Enhancement of Alongshore Freshwater
Transport in Surface-Advected River Plumes by
Tides. J. Phys. Oceanogr., 44, 2951–2971.
Epifanio, C.E., and
W. W. Garvine 2001 Larval transport on the Atlantic continental shelf
of North America: a review. Estuar. Coast.
Shelf Sci., 52, 51–77.
Fong, D. A., W. R.
Geyer, and R. P.
Signell 1997 The wind-forced response of a buoyant coastal
current: Observations of the western Gulf of
Maine plume, J. Mar. Syst., 12, 69–81
Fong, D. A.,
and W. R. Geyer 2001 Response of a river plume during an upwelling
favorable wind event. J. Geophys.
Res., 106, 1067–1084.
Fong, D., Geyer,
W.R. 2002 The alongshore transport of freshwater in a
surface-trapped river plume. J. Phys. Oceanogr.
32, 957–972.
Garvine, R. W. 2001 The impact of model configuration in studies of
buoyant coastal discharge, J. Mar.
Res., 59, 193–225.
Garvine, R. W. 1999 Penetration of buoyant coastal discharge onto
the continental shelf: A numerical model
experiment, J. Phys. Oceanogr., 29, 1892–1909.
Geyer, W. R., P. S. 2004 The transport, transformation and dispersal of
Hill, and G. C.
Kineke
sediment by buoyant coastal flows. Continental
Shelf Research, 24, 927–949.
Hickey, B., S.
Geier, N. Kachel,
and A. MacFadyen 2005 A bi-directional river plume: The Columbia in
summer. Cont. Shelf Res., 25, 1631–1656.
Lentz, S. J. 2001 The influence of stratification on the wind-
driven cross-shelf circulation over the North
Carolina Shelf. J. Phys. Oceanogr., 31, 2749–
2760.
Lentz, S. J.
2004
The response of buoyant coastal plumes to
upwelling-favorable winds. J. Phys.
Oceanogr., 34, 2458–2469.
Lentz, S. J. and J.
Largier 2006 The Influence of Wind Forcing on the
Chesapeake Bay Buoyant Coastal Current. J.
Phys. Oceanogr., 36, 1305–1316.
Masse, A. K., and
C. R. Murthy 1992 Analysis of the Niagara River plume dynamics,
J. Geophys. Res., 97, 2403-2420.
McGillicuddy Jr, 2003 A mechanism for offshore initiation of harmful
D. J., R. P. Signell,
C. A. Stock, B. A.
Keafer, M. D.
Keller, and R. D.
Hetland, and D. M.
Anderson
algal blooms in the coastal Gulf of Maine. J.
Plankton Res., 25(9): 1131-1138.
Moffat, C., and S.
J. Lentz 2012 On the response of a buoyant plume to
downwelling-favorable wind stress. J. Phys.
Oceanogr., 42, 1083–1098.
Rennie, S., S. J.
Lentz, and J.
Largier 1999 Observations of a pulsed buoyancy current
downstream of Chesapeake Bay. J. Geophys.
Res., 104 (C8), 18 227–18 240.
Souza, A. J., and J.
H. Simpson 1997 Controls on stratification in the Rhine
ROFI system, J. Mar. Syst., 12, 311-323.
Whitney, M. M.,
and R. W. Garvine, 2005 Wind influence on a coastal buoyant outflow. J.
Geophys. Res., 110, C03014.
dc.identifier.urihttp://tdr.lib.ntu.edu.tw/jspui/handle/123456789/52402-
dc.description.abstract2012 年,Moffat 和 Lentz 在二維的海洋模式中發現,在有沿岸淡水
(buoyant coastal current) 的情況下,致沉流風場 (downwelling-favorable wind) 能
夠於近岸側產生湧升環流 (upwelling circulation)。本研究利用 ROMS (Regional
Ocean Modeling System) 建立一三維模式,針對 Moffat 和 Lentz 提出之此一現
象進行敏感度測試和動力分析。本模式沿用 Moffat 和 Lent 的初始設定,設置固
定的淡水流量持續注入簡單斜坡地形上。當淡水沿著海岸形成細長的沿岸流後,
加入穩定向著沿岸流流向吹送的風場 (致沉流風場)。
與 Moffat 和 Lentz 的模式結果相同,一開始,致沉流風場造成下沉環流。
表面速度向岸,底部速度離岸的下沉環流使沿岸流之等密度線變陡。當等密度線
近乎垂直時,沿岸流的前緣卻產生湧升環流。而此湧升環流的強度會隨著淡水流
量的增加,坡度變陡和初始的淡海水密度差增加而增強。
由拆解沿岸速度,分成地轉流速和非地轉流速發現,當密度梯度造成的沿
岸地轉流切 (geostrophic shear) 大過風所能支持的速度切 (wind-supported shear)
時,即有表面速度離岸,底部速度向岸的湧升環流於密度梯度大處 (density front)
產生。此現象的發生是由於跨岸方向的壓力梯度力和柯氏力不平衡所導致。湧升
環流之表面離岸速度試圖減緩側向密度梯度和表面水位梯度,以減少表面大過於
科氏力的壓力梯度力。我們也利用了考慮側向密度梯度的 Ekman model 對應到
沿岸速度分析的結果:地轉流切和風應力所提供的速度切,兩者之相對大小會影
響跨向環流的方向和強度。
zh_TW
dc.description.abstractA two-dimensional modeling study by Moffat and Lentz (2012) showed that,in the presence of buoyant coastal currents, upwelling circulation could be generated under downwelling-favorable wind. The sensitivities and the dynamics of this upwelling circulation are studied using a three-dimensional ocean model (ROMS). The model is configured with a river source discharging onto a constant sloping shelf. After a slender of buoyant coastal currents develops, stable downwelling wind stress is applied.
Consistent with Moffat and Lentz (2012), downwelling wind stress initially produces downwelling circulation (i.e. onshore surface flow) that steepens the isopycanl and enhances the cross-shelf density gradient. When the isopycnals become nearly vertical, upwelling circulation is formed within the coastal currents. The circulation is strengthened by increasing discharge and increasing slope.
Analyses of decomposing along-shelf velocity into geostrophic and ageostrophic parts show that, the upwelling circulation forms when the geostrophic shear of alongshelf velocity due to cross-shelf density gradients is greater than the shear supported by wind. This indicates that cross-shore pressure gradient force and Coriolis force are imbalanced, and the surface offshore flow is induced to weaken the density gradient. A simple analytical Ekman model accounting for the cross-shelf density gradients is used to demonstrate the control of cross-shelf circulation by the relative strength of geostrophic shear and wind-supported shear.
en
dc.description.provenanceMade available in DSpace on 2021-06-15T16:13:51Z (GMT). No. of bitstreams: 1
ntu-103-R02241103-1.pdf: 2615957 bytes, checksum: 7d246c8510a4e2be0331821b4c4b905e (MD5)
Previous issue date: 2014
en
dc.description.tableofcontents致謝 ................................................................................................ i
摘要 ................................................................................................ii
Abstract ............................................................................................ iii
Contents .......................................................................................... iv
List of tables .................................................................................... vi
List of figures ................................................................................... vii
Chapter 1. Introduction ......................................................................... 1
1.1 Background .............................................................................. 1
1.2 Motivation ................................................................................. 2
Chapter 2. Method .............................................................................. 6
2.1 Numerical model ......................................................................... 6
2.2 Model Validation ........................................................................ 10
2.2.1 Classic Ekman model: momentum budget ........................................ 10
2.2.2 Classic Ekman model: velocity profile.......................................... 11
2.2.3 Numerical model ...................................................................... 12
Chapter 3. Result ................................................................................ 17
3.1 Cross-shore circulation ................................................................. 17
3.2 Sensitivity analyses ..................................................................... 23
3.3 Analytical Ekman model .............................................................. 30
3.3.1 Geostrophic and ageostrophic velocity .......................................... 30
3.3.2 Analytical solution ................................................................... 32
3.3.3 Comparison of analytical solution and numerical model .................... 34
3.4 Momentum analyses ...................................................................... 37
iv3.4.1 Along-shore ageostrophic velocity .................................................... 37
3.4.2 Force balance ......................................................................... 42
Chapter 4. Discussion ............................................................................ 47
4.1 Regime Diagram ............................................................................... 47
4.2 Adjustment time ............................................................................. 51
4.3 Prediction of ageostrophic cross-shore velocity ................................... 54
Chapter 5. Conclusion ............................................................................ 56
dc.language.isoen
dc.subject湧升環流zh_TW
dc.subject致沉流風場zh_TW
dc.subject沿岸流zh_TW
dc.subject地轉流切zh_TW
dc.subject風持切變zh_TW
dc.subjectbuoyant coastal currenten
dc.subjectwind-supported shearen
dc.subjectgeostrophic shearen
dc.subjectdownwelling-favorable winden
dc.subjectupwellingen
dc.title致沉流風場下湧升環流的生成機制zh_TW
dc.titleGeneration of upwelling circulation under downwelling-favorable wind in the presence of buoyant coastal currenten
dc.typeThesis
dc.date.schoolyear103-2
dc.description.degree碩士
dc.contributor.oralexamcommittee蔡武廷(Wu-ting Tsai),詹森(Sen Jan)
dc.subject.keyword湧升環流,致沉流風場,沿岸流,地轉流切,風持切變,zh_TW
dc.subject.keywordupwelling,downwelling-favorable wind,buoyant coastal current,geostrophic shear,wind-supported shear,en
dc.relation.page60
dc.rights.note有償授權
dc.date.accepted2015-08-18
dc.contributor.author-college理學院zh_TW
dc.contributor.author-dept海洋研究所zh_TW
顯示於系所單位:海洋研究所

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