Study on the spatiotemporal variation of the Yangtze estuarine tidal species

被引:6
作者
Gan, Min [1 ,2 ,3 ,4 ,5 ]
Chen, Yongping [3 ,4 ]
Pan, Haidong [6 ,7 ,8 ]
Pan, Shunqi [5 ]
Lai, Xijun [1 ,2 ]
Wen, Yuncheng [9 ]
Xia, Mingyan [9 ]
Zhang, Yinghao [1 ]
机构
[1] Chinese Acad Sci, State Key Lab Lake Sci & Environm, Nanjing Inst Geog & Limnol, Nanjing 210008, Peoples R China
[2] Chinese Acad Sci, Nanjing Inst Geog & Limnol, Poyang Lake Wetland Res Stn, Jiujiang 332899, Peoples R China
[3] Hohai Univ, Natl Key Lab Water Disaster Prevent, Nanjing 210098, Peoples R China
[4] Hohai Univ, Coll Harbour Coastal & Offshore Engn, Nanjing 210098, Peoples R China
[5] Cardiff Univ, Hydroenvironm Res Ctr, Sch Engn, Cardiff CF24 3AA, Wales
[6] Minist Nat Resources, Inst Oceanog 1, Qingdao 266061, Peoples R China
[7] Minist Nat Resources, Key Lab Marine Sci & Numer Modeling, Qingdao 266061, Peoples R China
[8] Pilot Natl Lab Marine Sci & Technol, Lab Reg Oceanog & Numer Modeling, Qingdao 266237, Peoples R China
[9] Nanjing Hydraul Res Inst, River & Harbor Engn Dept, Nanjing 210029, Peoples R China
基金
中国国家自然科学基金;
关键词
Tidal species; Estuarine tides; Yangtze estuary; VMD; NS_TIDE; HARMONIC-ANALYSIS; RIVER ESTUARY; WATER-LEVEL; NONSTATIONARY; DYNAMICS; CHANNEL; LINKING; PROPAGATION; EXPLORATION; MODEL;
D O I
10.1016/j.ecss.2024.108637
中图分类号
Q17 [水生生物学];
学科分类号
071004 ;
摘要
Owing to the nonlinear influence of river discharge, estuarine tides are nonstationary and more complicated than oceanic tides. This study investigated the spatiotemporal variation pattern of the Yangtze estuarine tides by considering tidal species separated using the Variational Mode Decomposition (VMD) model. The separated tidal species were compared with tidal species reconstructed using the NS_TIDE model. The results showed that the subtidal (D0) amplitude increased landward because of the enhanced influence of river discharge and river-tide interactions; diurnal (D1) and semi-diurnal (D2) tidal amplitudes consistently decayed landward because of frictional dissipation and nonlinear energy transfer to other tidal constituents; while quarter-diurnal (D4) and six-diurnal (D6) tidal amplitudes initially increased and then decreased in the landward direction because of the transformation of the dominant role of river discharge from nonlinear energy transfer to frictional dissipation. The spatiotemporal variations in different tidal species can illustrate other tidal processes, such as seasonal differences in tidal duration asymmetry. Although the VMD model neglects the separation of each tidal constituent, it can provide reasonable information, even when NS_TIDE may provide implausible results during the flood season because of the highly nonstationary conditions.
引用
收藏
页数:11
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