Global seamless tidal simulation using a 3D unstructured-grid model (SCHISM v5.10.0)

被引:11
|
作者
Zhang, Y. Joseph [1 ]
Fernandez-Montblanc, Tomas [2 ]
Pringle, William [3 ]
Yu, Hao-Cheng [1 ]
Cui, Linlin [1 ]
Moghimi, Saeed [4 ]
机构
[1] Virginia Inst Marine, Coll William & Mary Sci, Ctr Coastal Resource Management, Gloucester Point, VA 23062 USA
[2] Univ Cadiz, Earth Sci Dept, INMAR, Puerto Real 11519, Spain
[3] Argonne Natl Lab, Environm Sci Div, Lemont, IL 60439 USA
[4] NOAA Natl Ocean Serv, Coastal Survey Dev Lab, Silver Spring, MD 20910 USA
关键词
SEA-LEVEL RISE; CROSS-SCALE; OCEAN; CIRCULATION; COASTAL; DESIGN;
D O I
10.5194/gmd-16-2565-2023
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
We present a new 3D unstructured-grid global ocean model to study both tidal and nontidal processes, with a focus on the total water elevation. Unlike existing global ocean models, the new model resolves estuaries and rivers down to similar to 8 m without the need for grid nesting. The model is validated with both satellite and in situ observations for elevation, temperature, and salinity. Tidal elevation solutions have a mean complex root-mean-square error (RMSE) of 4.2 cm for M2 and 5.4 cm for all five major constituents in the deep ocean. The RMSEs for the other four constituents, S2, N2, K1, and O1, are, respectively, 2.05, 0.93, 2.08, and 1.34 cm). The nontidal residual assessed by a tide gauge dataset (GESLA) has a mean RMSE of 7 cm. For the first time ever, we demonstrate the potential for seamless simulation on a single mesh from the global ocean into several estuaries along the US West Coast. The model is able to accurately capture the total elevation, even at some upstream stations. The model can therefore potentially serve as the backbone of a global tide surge and compound flooding forecasting framework.
引用
收藏
页码:2565 / 2581
页数:17
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