期刊
出版社
ROYAL SOC
DOI: 10.1098/rsta.2017.0342
关键词
ocean waves; sea ice; attenuation; parametrization; power law fluid
资金
- ONR Departmental Research Initiative 'Sea State and Boundary Layer Physics of the Emerging Arctic Ocean' [N00014-131-0279]
- EU FP7 grant [SPA-2013.1.1-06]
- University of Otago
- EPSRC [EP/K032208/1]
- EPSRC [EP/R014604/1, EP/K032208/1] Funding Source: UKRI
Because of their capacity to alter floe size distribution and concentration and consequently to influence atmosphere-ocean fluxes, there is a compelling justification and demand to include waves in ice/ocean models and earth system models. Similarly, global wave forecasting models like WAVEWATCH III (R) need better parametrizations to capture the effects of a sea ice cover such as the marginal ice zone on incoming wave energy. Most parametrizations of wave propagation in sea ice assume without question that the frequency-dependent attenuation which is observed to occur with distance x travelled is exponential, i.e. A =A(0) e(-alpha x). This is the solution of the simple first-order linear ordinary differential equation dA/dx = -alpha A, which follows from an Airy wave mode ansatz A exp i(kx +/- omega t). Yet, in point of fact, it now appears that exponential decay may not be observed consistently and a more general equation of the type dA/dx = -alpha A(n) is proposed to allow for a broader range of attenuation behaviours should this be necessary to fit data. This article is part of the theme issue 'Modelling of sea-ice phenomena'.
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