Wave boundary layer model in SWAN revisited

被引:11
|
作者
Du, Jianting [1 ,3 ,4 ]
Bolanos, Rodolfo [2 ]
Larsen, Xiaoli Guo [1 ]
Kelly, Mark [1 ]
机构
[1] Tech Univ Denmark, Dept Wind Energy, Roskilde, Denmark
[2] DHI, Agern Alle 5, Horsholm, Denmark
[3] Minist Nat Resources China, Inst Oceanog 1, Qingdao, Shandong, Peoples R China
[4] Qingdao Natl Lab Marine Sci & Technol, Lab Reg Oceanog & Numer Modeling, Qingdao, Shandong, Peoples R China
基金
欧盟地平线“2020”;
关键词
SOURCE TERMS; DISSIPATION; EVOLUTION; BREAKING;
D O I
10.5194/os-15-361-2019
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
In this study, we extend the work presented in Du et al. (2017) to make the wave boundary layer model (WBLM) applicable for real cases by improving the wind-input and white-capping dissipation source functions. Improvement via the new source terms includes three aspects. First, the WBLM wind-input source function is developed by considering the impact of wave-induced wind profile variation on the estimation of wave growth rate. Second, the white-capping dissipation source function is revised to be not explicitly dependent on wind speed for real wave simulations. Third, several improvements are made to the numerical WBLM algorithm, which increase the model's numerical stability and computational efficiency. The improved WBLM wind-input and white-capping dissipation source functions are calibrated through idealized fetch-limited and depth-limited studies, and validated in real wave simulations during two North Sea storms. The new WBLM source terms show better performance in the simulation of significant wave height and mean wave period than the original source terms.
引用
收藏
页码:361 / 377
页数:17
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