By vertical boundary conditions, a spectral expansion of horizontal tide wave velocity is done in vertical direction in terms of a complete basis functions selected properly, hence a relation between tide levels and...By vertical boundary conditions, a spectral expansion of horizontal tide wave velocity is done in vertical direction in terms of a complete basis functions selected properly, hence a relation between tide levels and spectral components is found theoretically under condition of ignoring the horizontal friction stress and nonlinear effect. And a relation between bottom friction of tide current, which satisfies the viscous condition on sea bottom, and tide levels is determined. The relation is different from the relation of the traditional parameterizing of bottom friction. Moreover integration of the continuity equation and momentum equations is carried out in the vertical direction using zero flux condition on solid boundaries and inputting condition on open boundaries, and then a boundary value problem of elliptic form on the tide levels is constructed.展开更多
潟湖体系的潮汐动力对其地貌演变、生态环境保护与海岸带资源的可持续开发利用等具有重要影响。以广东惠州双月湾潟湖为研究靶区,基于2020—2023年4次潮位观测资料,采用基于光滑导纳原理的短时调和分析(modified harmonic analysis mode...潟湖体系的潮汐动力对其地貌演变、生态环境保护与海岸带资源的可持续开发利用等具有重要影响。以广东惠州双月湾潟湖为研究靶区,基于2020—2023年4次潮位观测资料,采用基于光滑导纳原理的短时调和分析(modified harmonic analysis model on the basis of the credo of smoothness,MHACS)模型和数理统计方法初步探讨该潟湖体系潮波传播和变化过程。结果表明,双月湾潟湖体系平均潮差为0.52~0.69m,潮波从口门传播至潟湖上段,其能量明显减小,特别是上游区域的潮波衰减率为近口门段20倍,潮波传播速度亦降低至近口门段的12%。在潟湖中,半日潮M2、全日潮K1和浅水潮M4占据主导,其振幅分别为23.06cm、30.4cm和7.74cm。其中,全日潮和半日潮的振幅月变化较为稳定,而浅水分潮的季节波动更加明显,尤其是向上游传播时,分潮的振幅和迟角季节性变化更为显著。潮波通过口门传入双月湾潟湖,受地形辐聚与底床摩擦效应影响,不同河段的潮波传播速度差异显著,尤其是半日潮在口门区的传播速度普遍高于全日潮。各分潮在潟湖内的振幅衰减明显,特别是S2、M4和MS4分潮的振幅梯度最为显著(4×10^(−6)m^(−1))。展开更多
文摘By vertical boundary conditions, a spectral expansion of horizontal tide wave velocity is done in vertical direction in terms of a complete basis functions selected properly, hence a relation between tide levels and spectral components is found theoretically under condition of ignoring the horizontal friction stress and nonlinear effect. And a relation between bottom friction of tide current, which satisfies the viscous condition on sea bottom, and tide levels is determined. The relation is different from the relation of the traditional parameterizing of bottom friction. Moreover integration of the continuity equation and momentum equations is carried out in the vertical direction using zero flux condition on solid boundaries and inputting condition on open boundaries, and then a boundary value problem of elliptic form on the tide levels is constructed.
文摘潟湖体系的潮汐动力对其地貌演变、生态环境保护与海岸带资源的可持续开发利用等具有重要影响。以广东惠州双月湾潟湖为研究靶区,基于2020—2023年4次潮位观测资料,采用基于光滑导纳原理的短时调和分析(modified harmonic analysis model on the basis of the credo of smoothness,MHACS)模型和数理统计方法初步探讨该潟湖体系潮波传播和变化过程。结果表明,双月湾潟湖体系平均潮差为0.52~0.69m,潮波从口门传播至潟湖上段,其能量明显减小,特别是上游区域的潮波衰减率为近口门段20倍,潮波传播速度亦降低至近口门段的12%。在潟湖中,半日潮M2、全日潮K1和浅水潮M4占据主导,其振幅分别为23.06cm、30.4cm和7.74cm。其中,全日潮和半日潮的振幅月变化较为稳定,而浅水分潮的季节波动更加明显,尤其是向上游传播时,分潮的振幅和迟角季节性变化更为显著。潮波通过口门传入双月湾潟湖,受地形辐聚与底床摩擦效应影响,不同河段的潮波传播速度差异显著,尤其是半日潮在口门区的传播速度普遍高于全日潮。各分潮在潟湖内的振幅衰减明显,特别是S2、M4和MS4分潮的振幅梯度最为显著(4×10^(−6)m^(−1))。
