Message Board

Respected readers, authors and reviewers, you can add comments to this page on any questions about the contribution, review, editing and publication of this journal. We will give you an answer as soon as possible. Thank you for your support!

Full name
E-mail
Phone number
Title
Message
Verification Code
Volume 42 Issue 11
Dec.  2020
Turn off MathJax
Article Contents
Chen Yugeng,Bao Xianwen,Zhou Lingling, et al. Global tidal current energy assessment based on unstructured mesh model[J]. Haiyang Xuebao,2020, 42(11):23–33 doi: 10.3969/j.issn.0253-4193.2020.11.003
Citation: Chen Yugeng,Bao Xianwen,Zhou Lingling, et al. Global tidal current energy assessment based on unstructured mesh model[J]. Haiyang Xuebao,2020, 42(11):23–33 doi: 10.3969/j.issn.0253-4193.2020.11.003

Global tidal current energy assessment based on unstructured mesh model

doi: 10.3969/j.issn.0253-4193.2020.11.003
  • Received Date: 2019-09-25
  • Rev Recd Date: 2020-01-08
  • Available Online: 2020-12-08
  • Publish Date: 2020-11-25
  • Using the Finite-Volume Community Ocean Model (FVCOM) numerical model, considering the combination of parameterization of internal tidal dissipation and self-attraction and loading tide in the unstructured mesh model for the first time, a total of six tide-generation forces including M2、S2、N2、K1、O1、Q1 are established to drive the global forward tidal model. Based on the verification of the global tidal model results, we calculate and statistically estimate average density of the global tidal current energy, and show the tidal current energy distributions where there is greater tidal current energy in the world. The results show that there is a large tidal current energy belt with an area of nearly 33 000 $ {{\rm{k}}{\rm{m}}}^{2} $ and a maximum tidal current energy density of 1 100 $ {\rm{W}}/{{\rm{m}}}^{2} $ in the English Channel. The maximum tidal current energy density in the western side of Baffin Island in Canada exceeds 1 150 $ {\rm{W}}/{{\rm{m}}}^{2} $. The maximum tidal current energy density in the Cook Bay waters of Alaska is 500 $ {\rm{W}}/{{\rm{m}}}^{2} $. The tidal current energy belt at the entrance to the White Sea in Russia is large, where the maximum tidal current energy density reaches 500 $ {\rm{W}}/{{\rm{m}}}^{2} $. Australia's coastal tidal current energy belts have small area but large amount, and their tidal current energy density generally exceed 100 $ {\rm{W}}/{{\rm{m}}}^{2} $. In China's offshore waters, the tidal current energy density in the Hangzhou Bay waters of the Changjiang River Estuary and the north of Taipei reaches 100 $ {\rm{W}}/{{\rm{m}}}^{2} $.
  • loading
  • [1]
    Renewable Energy Policy Network for the 21st Century. Renewables 2018 Global Status Report[R/OL]. (2018-07-18)[2019-05-11]. http://www.buildup.eu/en/node/56128.
    [2]
    段自豪, 陈正寿. 潮流发电现状分析及未来展望[J]. 中国水运(下半月), 2012, 12(2): 106−107, 145.

    Duan Zihao, Chen Zhengshou. Current situation analysis and future prospect of tidal current power generation[J]. China Water Transport, 2012, 12(2): 106−107, 145.
    [3]
    张理, 李志川. 潮流能开发现状、发展趋势及面临的力学问题[J]. 力学学报, 2012, 48(5): 1019−1032.

    Zhang Li, Li Zhichuan. Development status, trend and the problems of mechanics of tidal current energy[J]. Chinese Journal of Theoretical and Applied Mechanics, 2012, 48(5): 1019−1032.
    [4]
    水电与新能源期刊编辑部. 国内外新能源开发资料选登[J]. 水电与新能源, 2018, 32(10): 79−80.

    Editorial Department of Journal of hydropower and new energy. New energy development materials at home and abroad[J]. Hydropower and New Energy, 2018, 32(10): 79−80.
    [5]
    Pekeris C L, Accad Y. Solution of Laplace’s equations for the M2 tide in the world oceans[J]. Philosophical Transactions of the Royal Society of London, 1969, 265(1165): 413−436.
    [6]
    Schwiderski E W. On charting global ocean tides[J]. Reviews of Geophysics, 1980, 18(1): 243−268. doi: 10.1029/RG018i001p00243
    [7]
    Stammer D, Ray R D, Andersen O B, et al. Accuracy assessment of global barotropic ocean tide models[J]. Reviews of Geophysics, 2014, 52(3): 243−282. doi: 10.1002/2014RG000450
    [8]
    Chen C, Liu H, Beardsley R C. An unstructured grid, finite-volume, three-dimensional, primitive equations ocean model: application to coastal ocean and estuaries[J]. Journal of Atmospheric and Oceanic Technology, 2003, 20: 159−186. doi: 10.1175/1520-0426(2003)020<0159:AUGFVT>2.0.CO;2
    [9]
    Egbert G D, Ray R D. Significant dissipation of tidal energy in the deep ocean inferred from satellite altimeter data[J]. Nature, 2000, 405(6788): 775−778.
    [10]
    Egbert G D, Ray R D. Estimates of M2 tidal energy dissipation from TOPEX/Poseidon altimeter data[J]. Journal of Geophysical Research Oceans, 2001, 106(C10): 22475−22502. doi: 10.1029/2000JC000699
    [11]
    Jayne S R, St Laurent L C. Parameterizing tidal dissipation over rough topography[J]. Geophysical Research Letters, 2001, 28(5): 811−814. doi: 10.1029/2000GL012044
    [12]
    Ray R D. Ocean self-attraction and loading in numerical tidal models[J]. Marine Geodesy, 1998, 21(3): 181−192. doi: 10.1080/01490419809388134
    [13]
    Farrell W E. Deformation of the Earth by surface loads[J]. Reviews of Geophysics, 1972, 10(3): 761−797.
    [14]
    Arbic B K, Garner S T, Hallberg R W, et al. The accuracy of surface elevations in forward global barotropic and baroclinic tide models[J]. Deep-Sea Research Part II, 2004, 51(25/26): 3069−3101.
    [15]
    Egbert G D, Gary D. Numerical modeling of the global semidiurnal tide in the present day and in the last glacial maximum[J]. Journal of Geophysical Research, 2004, 109(C3): C03003.
    [16]
    Iyer A S, Couch S J, Harrison G P, et al. Variability and phasing of tidal current energy around the United Kingdom[J]. Renewable Energy, 2013, 51: 343−357. doi: 10.1016/j.renene.2012.09.017
  • 加载中

Catalog

    通讯作者: 陈斌, bchen63@163.com
    • 1. 

      沈阳化工大学材料科学与工程学院 沈阳 110142

    1. 本站搜索
    2. 百度学术搜索
    3. 万方数据库搜索
    4. CNKI搜索

    Figures(18)  / Tables(4)

    Article views (249) PDF downloads(48) Cited by()
    Proportional views
    Related

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return