Third-order WENO transport scheme for simulating the baroclinic eddying ocean on an unstructured grid. (November 2019)

• Record Type: Journal Article
• Authors: Ye, Fei; Zhang, Yinglong J.; He, Ruoying; Wang, Zhengui; Wang, Harry V.; Du, Jiabi
• Is Part Of: Ocean modelling. Volume 143(2019)
• Publication Date: 2019-11
• Subjects: SCHISM -- Eddying regime -- WENO -- Baroclinic -- Gulf stream; Oceanography -- Periodicals; Océanographie -- Périodiques; Oceanography; Periodicals; 551.46
• DOI: 10.1016/j.ocemod.2019.101466
• Languages: English
• ISSNs: 1463-5003

Abstract

Abstract: Despite the recent success achieved by the unstructured-grid SCHISM (Semi-implicit Cross-scale Hydroscience Integrated System Model) in multi-resolution studies, its skill in simulating the baroclinic eddying ocean needs to be further improved. In particular, the classical 2nd-order transport schemes for estuaries and coastal zones are too dissipative to resolve the baroclinic dynamics associated with strong boundary currents, such as meso-scale meanders and eddies. To close this gap, this paper presents a newly designed 3rd-order finite volume transport scheme, based on the Weighted Essentially Non-Oscillatory (WENO) formalism. This new scheme strikes a delicate balance among accuracy, efficiency, and monotonicity for the transport in the eddying regime. Idealized numerical benchmark experiments demonstrate that the WENO scheme is very effective in limiting numerical diffusion. The scheme is then applied in a realistic simulation of the Gulf Stream and the surrounding circulation, further confirming its capability of resolving baroclinic meso-scale eddies and meanders. This new high-order transport scheme is therefore ideal for extending the ability of SCHISM to study cross-scale baroclinic applications that range from the river dynamics to the eddying ocean processes. Highlights: A new 3rd -order transport scheme based on WENO is developed for unstructured grids. The new scheme balances among accuracy, efficiency, monotonicity for eddying regime. Mesoscale eddies and meanders of the Gulf Stream are qualitatively captured.