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海浪-海流-海冰相互作用對西北大西洋上層海洋的影響研究

海浪-海流-海冰相互作用對西北大西洋上層海洋的影響研究

作者:林尚飛著
出版社:河海大學(xué)出版社出版時(shí)間:2023-03-01
開本: 24cm 頁數(shù): 231頁
中 圖 價(jià):¥69.1(7.2折) 定價(jià)  ¥96.0 登錄后可看到會(huì)員價(jià)
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海浪-海流-海冰相互作用對西北大西洋上層海洋的影響研究 版權(quán)信息

  • ISBN:9787563082117
  • 條形碼:9787563082117 ; 978-7-5630-8211-7
  • 裝幀:一般膠版紙
  • 冊數(shù):暫無
  • 重量:暫無
  • 所屬分類:>

海浪-海流-海冰相互作用對西北大西洋上層海洋的影響研究 內(nèi)容簡介

本書研究了海浪-海流-海冰相互作用中的重要物理過程對西北大西洋上層物理環(huán)境的影響及其動(dòng)力機(jī)制。首先通過建立海浪-海流-海冰的單向耦合模型,研究在海流和海冰影響下的波浪成長、耗散及傳播?紤]波浪對海氣交換的影響,基于觀測資料發(fā)現(xiàn)了不同海況下海表粗糙度關(guān)于波齡的不同關(guān)系,提出并驗(yàn)證了新的海表粗糙度參數(shù)化方案。針對波浪淺水破碎的過程,提出并驗(yàn)證了破碎指標(biāo)關(guān)于地形坡度的非線性公式。上述參數(shù)化方案被用于首個(gè)西北大西洋波流全耦合模型,研究了颶風(fēng)期間西北大西洋的波流相互作用過程。結(jié)果表明波流相互作用顯著改變著海洋表層水動(dòng)力,且能夠影響到上百米水深。波致應(yīng)力、波浪混合、波浪增強(qiáng)的風(fēng)應(yīng)力和底摩阻在不同的條件下對海洋環(huán)境都能起到主導(dǎo)作用,因而其影響對復(fù)雜多變的海洋都是不容忽略的。

海浪-海流-海冰相互作用對西北大西洋上層海洋的影響研究 目錄

ABSTRACT ACKNOWLEDGEMENTS CHAPTER 1 INTRODUCTION 1.1 Background 1.1.1 Ocean Surface Wave 1.1.2 Wave-Ice Interactions 1.1.3 Wave-Current Interactions 1.2 Objectives 1.3 Outline CHAPTER 2 PERFORMANCES OF VISCOELASTIC MODELS FOR OCEAN WAVE DISSIPATION IN ICE-COVERED REGIONS 2.1 Introduction 2.2 Methodology 2.2.1 Spectral Wave Model and Wave Dissipation in Ice 2.2.2 Wave Model Setup 2.2.3 Model Forcing 2.2.4 Wind and Wave Observations 2.3 Model Validations 2.3.1 Wind Forcing 2.3.2 Significant Wave Height 2.3.3 Peak Wave Period 2.4 Results 2.4.1 Determination of Ice Rheological Parameters 2.4.2 Comparisons of Two Viscoelastic Models for Wave Dissipation 2.4.3 Effects of Wave Scattering on Wave Propagations 2.5 Discussion 2.6 Conclusions CHAPTER 3 DEPENDENCES OF DRAG COEFFICIENT ON WIND SPEED AND WAVE STATE 3.1 Introduction 3.2 Drag Coefficient at the Sea Surface 3.3 Observational Data 3.3.1 FETCH 3.3.2 GOTEX 3.3.3 Grand Banks Experiment 3.3.4 HEXMAX 3.3 . J North Sea Experiment 3.3.6 RASEX 3.3.7 SWADE 3.3.8 WAVES 3.4 Analyses of Observational Wind Stress and Wave Data 3.4.1 Wind-speed-dependent Drag Coefficient 3.4.2 Wave-dependent Drag Coefficient 3.4.3 A New Parameterization of the Drag Coefficient 3.4.4 Assessment of Existing and New Parameterizations 3.5 Wave Simulations Using Different Drag Coefficient Parameterizations 3.5.1 Spectral Wave Model and Setup 3.5.2 Model Forcing 3.5.3 Wind and Wave Observations 3.5.4 Wave Model Results 3.6 Discussion and Conclusions CHAPTER 4 PERFORMANCES OF WAVE BREAKING PARAME-TERIZATIONS IN THE SPECTRAL WAVE MODEL 4.1 Introduction 4.2 Model Description and Depth-induced Wave Breaking Parameterizations 4.2.1 Spectral Wave Model 4.2.2 Existing Parameterizations for Depth-induced Wave Breaking 4.2.3 A New Parameterization for Depth-induced Wave Breaking 4.3 Observational Data and Methodology 4.3.1 Laboratory and Field Observations 4.3.2 Wave Model Setup 4.4 Results and Discussion 4.4.1 Performances of Six Existing Parameterizations 4.4.2 Effect of Bottom Slope and Normalized Water Depth 4.4.3 Calibration and Validation of the New Parameterization 4.5 Conclusions CHAPTER 5 WAVE-CURRENT INTERACTIONS DURING HURRI- CANES EARL AND IGOR 5.1 Introduction 5.2 The Coupled Wave-Circulation Model 5.2.1 Ocean Wave Model 5.2.2 Ocean Circulation Model 5.2.3 Model Configurations 5.3 Observational Data 5.4 Hurricanes Earl and Igor 5.5 Effects of Currents on Waves 5.5.1 Significant Wave Height 5.5.2 Peak Wave Period 5.5.3 Wave Spectra 5.5.4 Maximum Significant Wave Height 5.6 Effects of Waves on Circulations 5.6.1 Sea Level 5.6.2 Sea Surface Current 5.6.3 Sea Surface Salinity 5.6.4 Sea Surface Temperature 5.6.5 Vertical Structure of Temperature 5.7 Summary and Conclusions CHAPTER 6 CONCLUSIONS 6.1 Main Results and Their Significance 6.2 Future Work APPENDIX A STATISTICS FOR MODEL COMPARISONS APPENDIX B DEPENDENCES OF WAVE DISSIPATION ON ICE AND WAVE PROPERTIES BIBLIOGRAPHY
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