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

<p>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 <span class="inline-formula">∼8</span&g...

Full description

Bibliographic Details
Published in:Geoscientific Model Development
Main Authors: Y. J. Zhang, T. Fernandez-Montblanc, W. Pringle, H.-C. Yu, L. Cui, S. Moghimi
Format: Article
Language:English
Published: Copernicus Publications 2023-05-01
Online Access:https://gmd.copernicus.org/articles/16/2565/2023/gmd-16-2565-2023.pdf
Description
Summary:<p>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 <span class="inline-formula">∼8</span> 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.</p>
ISSN:1991-959X
1991-9603