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Exponential distribution of wave-driven near-bed water speeds under short-crested waves: a case study in the eastern Gulf of Riga, the Baltic Sea
被引:1
|作者:
Eelsalu, Maris
[1
]
Piho, Laura
[2
]
Aigars, Juris
[3
]
Kelpsaite-Rimkiene, Loreta
[4
]
Kondrat, Vitalijus
[4
]
Kruusmaa, Maarja
[2
]
Parnell, Kevin E.
[1
]
Ristolainen, Asko
[2
]
Sakurova, Ilona
[4
]
Skudra, Maris
[3
]
Viska, Maija
[3
]
Soomere, Tarmo
[1
,5
]
机构:
[1] Tallinn Univ Technol, Sch Sci, Dept Cybernet, Wave Engn Lab, Ehitajate Tee 5, EE-19086 Tallinn, Estonia
[2] Tallinn Univ Technol, Ctr Biorobot, Sch Informat Technol, Ehitajate Tee 5, EE-19086 Tallinn, Estonia
[3] Latvian Inst Aquat Ecol, Voleru Iela 4, LV-1007 Riga, Kurzemes Rajons, Latvia
[4] Klaipeda Univ, Marine Res Inst, Herkaus Manto G 84, LT-92294 Klaipeda, Lithuania
[5] Estonian Acad Sci, Kohtu 6, EE-10130 Tallinn, Estonia
关键词:
wave loads;
wave climate;
near-bottom;
velocity;
water speed;
hydromast;
in-situ;
measurements;
ADV;
Weibull distribution;
HEIGHT;
STATISTICS;
VELOCITIES;
HINDCAST;
MODEL;
WIND;
PART;
D O I:
10.3176/proc.2025.1.03
中图分类号:
O [数理科学和化学];
P [天文学、地球科学];
Q [生物科学];
N [自然科学总论];
学科分类号:
07 ;
0710 ;
09 ;
摘要:
Loads exerted to the seabed by short-crested wind-seas with a wide directional spread have extensive spatio-temporal variability. We quantify this variability in terms of near-bed water speed using an array of nine high-resolution hydromast devices for recording pressure and water velocity in the range of 0.12-1 m/s mounted at a distance of 10 m from each other on a rigid rectangular frame of 20 x 20 m in approximately 4 m deep water and 700 m from the eastern shore of the Gulf of Riga near Skulte (Latvia) in August-September 2022. This array is complemented by an acoustic Doppler velocimeter (ADV). The average background current is very weak, approximately 0.003 m/s in the measurement location. The empirical distributions of velocity components are symmetric but greatly deviate from the expected Gaussian distribution. The empirical distributions of water speeds follow an exponential distribution rather than a Rayleigh or Forristall distribution. This shape of the distributions appears in the range of 0.2-0.7 m/s while the maximum speed reaches 1.22 m/s. The rate parameter (inverse scale parameter) varies almost by a factor of two in recordings by different devices. The recordings make it possible to identify wakes of vessels entering to or departing from the Port of Skulte.
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页码:23 / 42
页数:20
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