Tidal energy budget in the Zhujiang (Pearl River) Estuary

被引:0
作者
Peng Bai
Yanzhen Gu
Peiliang Li
Kejian Wu
机构
[1] Ocean University of China,Physical Oceanography Laboratory
[2] Ocean University of China,College of Information Science and Engineering
来源
Acta Oceanologica Sinica | 2016年 / 35卷
关键词
tidal energy flux; energy dissipation; Zhujiang Estuary; regional ocean modeling system;
D O I
暂无
中图分类号
学科分类号
摘要
Tidal energy budget in the Zhujiang (Pearl River) Estuary (ZE) is evaluated by employing high-resolution baroclinic regional ocean modeling system (ROMS). The results obtained via applying the least square method on the model elevations are compared against the tidal harmonic constants at 18 tide stations along the ZE and its adjacent coast. The mean absolute errors between the simulation and the observation of M2, S2, K1 and O1 are 4.6, 2.8, 3.2 and 2.8 cm in amplitudes and 9.8°, 15.0°, 4.6° and 4.6° in phase-lags, respectively. The comparisons between the simulated and observed sea level heights at 11 tide gauge stations also suggest good model performance. The total tidal energy flux incoming the ZE is estimated to be 343.49 MW in the dry season and larger than 336.18 MW in the wet season, which should due to higher mean sea level height and heavier density in the dry season. M2, K1, S2, O1 and N2, the top five barotropic tidal energy flux contributors for the ZE, import 242.23 (236.79), 52.97 (52.08), 24.49 (23.96), 16.22 (15.91) and 7.10 (6.97) MW energy flux into the ZE in dry (wet) season, successively and respectively. The enhanced turbulent mixing induced by eddies around isolated islands and sharp headlands dominated by bottom friction, interaction between tidal currents and sill topography or constricted narrow waterways together account for the five energy dissipation hotspots, which add up to about 38% of the total energy dissipation inside the ZE.
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页码:54 / 65
页数:11
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  • [1] Carbajal N(1998)Simulation of tides, residual flow and energy budget in the Gulf of California Oceanologica Acta 21 429-446
  • [2] Backhaus J O(2009)Numerical study of the tides and residual currents in the Qiongzhou Strait Chinese Journal of Oceanology and Limnology 27 931-942
  • [3] Chen C(1997)Simulation of barotropic and baroclinic tides off northern British Columbia Journal of Physical Oceanography 27 762-781
  • [4] Li P(2004)Seasonal variation and dynamics of the Pearl River plume Continental Shelf Research 24 1761-1777
  • [5] Shi M(1999)Numerical simulation of principal tidal constituents in the South China Sea, Gulf of Tonkin and Gulf of Thailand Continental Shelf Research 19 845-869
  • [6] Cummins P F(1999)Stratified flow over topography: the role of small-scale entrainment and mixing in flow establishment Proceedings of the Royal Society of London Series A: Mathematical Physical and Engineering Sciences. The Royal Society 455 3221-3258
  • [7] Oey L Y(1980)Circulation and energetics of a deep, strongly stratified inlet Canadian Journal of Fisheries and Aquatic Sciences 37 1398-1410
  • [8] Dong L(2009)Interaction of a river plume with coastal upwelling in the northeastern South China Sea Continental Shelf Research 29 728-740
  • [9] Su J(2008)Physical–biological coupling in the Pearl River Estuary Continental Shelf Research 28 1405-1415
  • [10] Wong L A(2011)Process study of circulation in the Pearl River Estuary and adjacent coastal waters in the wet season using a triply-nested circulation model Ocean Modelling 38 138-160