Representation of microscale ocean wavenumber spectrum correct to the second order

In this paper, the analytical representations of four wave source functions in high-frequency spectrum range are given on the basis of ocean wave theory and dimensional analysis, and the perturbation method is used to solve the governing equations of ocean wave high-frequency spectrum on the basis of the temporally stationary and locally homogeneous scale relations of microscale wave. The microscale ocean wavenumber spectrum correct to the second order has an explicit structure, its first order part represents the equilibrium between different source functions, and its second order part represents the contribution of microscale wave propagation.

作 者： YUAN Yeli HUA Feng   作者單位： YUAN Yeli(Key Laboratory of Marine Science and Numerical Modeling, State Oceanic Administration, Qingdao 266061, China)

HUA Feng(Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China;Key Laboratory of Marine Science and Numerical Modeling, State Oceanic Administration, Qingdao 266061, China;Graduate School of the Chinese Academy of Sciences, Beijing 100039, China) 

刊 名： 中國(guó)科學(xué)D輯（英文版）  SCI 英文刊名： SCIENCE IN CHINA SERIES D: EARTH SCIENCES  年，卷(期)： 2005 48(4)  分類號(hào)： P3  關(guān)鍵詞： temporally stationary and locally homogeneous   source function in high-frequency spectrum range   microscale ocean wavenumber spectrum  

【Representation of microscale ocean w】相關(guān)文章：

Projections of ocean climate for northwestern Pacific Ocean04-29

The Comprehension and Representation in the Translation of English Idioms04-29

Phonological Representation for Second Language Learners04-28

Angular Momentum Phase State Representation for Quantum Pendulum04-29

NUMERICAL MODELLING OF THE QUASI-GLOBAL OCEAN CIRCULATION BASED ON POM04-27

Contents and benthic fluxes of nutrients in sediment pore water of the Southern Ocean04-27

DECOMPOSITIONS OF BOSONIC MODULES OF LIE ALGEBRAS W1+∞ AND W1+∞(glN)04-29

Adaptability of the ocean and earth tidal models based on global observations of the superconducting gravimeters04-29

Physical mechanism and numerical simulations of surface layer temperature inversion in tropical ocean04-29

天文術(shù)語(yǔ) W-Z05-04