nerc.ac.uk

Proudman resonance with tides, bathymetry and variable atmospheric forcings

Williams, David A.; Horsburgh, Kevin J. ORCID: https://orcid.org/0000-0003-4803-9919; Schultz, David M.; Hughes, Chris W.. 2020 Proudman resonance with tides, bathymetry and variable atmospheric forcings. Natural Hazards. 10.1007/s11069-020-03896-y

Before downloading, please read NORA policies.
[thumbnail of Williams2020_Article_ProudmanResonanceWithTidesBath.pdf]
Preview
Text
Williams2020_Article_ProudmanResonanceWithTidesBath.pdf - Published Version
Available under License Creative Commons Attribution 4.0.

Download (2MB) | Preview

Abstract/Summary

Proudman resonance is a primary amplification mechanism for meteotsunamis, which are shallow-water waves generated by atmospheric forcings. The effect of tides, sloping bathymetry and the speed, amplitude and aspect ratio of the atmospheric forcing on Proudman resonant wave growth are investigated using analytical approximations and numerical models. With tides included, maximum wave growth through Proudman resonance occurred when the atmospheric-forcing speed matched the tidal-wave speed. Growth greater than Proudman resonance occurred with a positive tidal elevation together with a tidal current in the opposite direction to wave propagation, due to linear growth combined with further amplification from wave-flux conservation. Near-Proudman resonant growth occurred when the forced-wave speed or free-wave speed varied by either a small amount, or varied rapidly, around a speed appropriate for Proudman resonance. For a forcing moving at Proudman resonant speed, resultant wave growth was proportional to the total, time-integrated forcing amplitude. Finally, Proudman resonant wave growth was lower for forcings with lower aspect ratios (AP), partly because forced-wave heights are proportional to 1 + A 2P , but also because free waves could spread in two dimensions. Whilst the assumptions of strict Proudman resonance are never met, near-Proudman resonant growth may occur over hundreds of kilometres if the effective Froude number is near 1 and the resultant wave propagates predominantly in one dimension.

Item Type: Publication - Article
Digital Object Identifier (DOI): 10.1007/s11069-020-03896-y
ISSN: 0921-030X
Date made live: 14 May 2020 13:29 +0 (UTC)
URI: https://nora.nerc.ac.uk/id/eprint/527720

Actions (login required)

View Item View Item

Document Downloads

Downloads for past 30 days

Downloads per month over past year

More statistics for this item...