Effects of scattering and resonance on energy dissipation of an internal tide in a narrow shelf

• Published in: Journal of oceanography Vol. 63; no. 1; pp. 15 - 25
• Main Authors: Kawamura, Yuji, Kitade, Yujiro
• Format: Journal Article
• Language: English
• Published: Tokyo Springer Nature B.V 01.02.2007
• Subjects: Energy dissipation; Internal waves; Resonance
• ISSN: 0916-8370; 1573-868X
• DOI: 10.1007/s10872-007-0002-0

The effects of scattering and resonance on the energy dissipation of an internal tide were investigated using a two-dimensional model which is a reassembled version of the theoretical generation model devised by Rattray et al. (1969) for internal tide. The basic character of the scattering process at the step bottom was first investigated with a wide shelf model. When the internal wave incited from a deep region (Region II) into the shallow shelf region (Region I), a passing wave into the shallow region, a reflected wave into the deep region, and a beam-like wave, i.e. a scattered wave (SW), emanated at the step bottom. The SW, which consists of the superposition of numerous internal modes, propagated upward/downward into both regions. The general properties of the SW were well expressed around the shelf edge, even in the present model with viscosity effect. The amplitude of the SW decreased dramatically when the depth of the velocity maximum of the incident internal wave in Region II corresponded with the depth of the shelf edge. In the narrow shelf model, where the decay distance of the internal wave in Region I is longer than the shelf width, the incident internal wave reflected at the coast to form a standing wave. When the internal wave in Region I is enhanced by the resonance, the energy of the SW in Region II is also intensified. Furthermore, the energy of the modes in Region II predominated when the velocity maximum is identical to that of the dominant mode in Region I. These results suggest that the spatial scale of shelf region is a very important factor governing the energy dissipation of the internal tide through reflection and scattering in a narrow shelf.[PUBLICATION ABSTRACT]