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摘要:
The effect of the surface gravity waves over sea surface roughness length (z0) is investigated from several idealized numerical experiments with the Wave-Watch-III (WW3) model. The WW3 model is combined with a simplified model to estimate z0, CD, u* and U10 as function of the sea state. The impacts related to the presence of the ocean waves over z0 are obtained from conditions of growing (young waves) and mature seas (old waves). The wave spectrum is obtained from WW3 model for each idealized simulation under uniform wind conditions. Uniform wind experiments range from 15 to 45 m/s. The simplified algorithm determines z0, CD, u* and U10 for cases of young waves, old waves and by the Charnock method. The results show that when the ocean is characterized by young waves, both z0 and CD (drag coefficient) increase while U10 is reduced. In Charnock case, the values of z0, CD and U10 have no dependence with the presence of gravity waves. Experiments using winds higher than 30 m/s result in young waves’ CD values higher than the CD value for old waves. Even for young waves CD values are high for cases of strong winds. The results also show that in experiments using winds higher than 30 m/s the dependence between CD and wave age becomes stronger, which is in accordance with other studies.
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篇名 Impact of the Waves on the Sea Surface Roughness under Uniform Wind Conditions: Idealized Cases for Uniform Winds (Part I)
来源期刊 大气和气候科学(英文) 学科 数学
关键词 Surface GRAVITY WAVES Wind Sea OCEAN WAVES YOUNG WAVES OLD WAVES
年,卷(期) dqhqhkxyw_2015,(3) 所属期刊栏目
研究方向 页码范围 317-325
页数 9页 分类号 O1
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Surface
GRAVITY
WAVES
Wind
Sea
OCEAN
WAVES
YOUNG
WAVES
OLD
WAVES
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研究分支
研究去脉
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相关学者/机构
期刊影响力
大气和气候科学(英文)
季刊
2160-0414
武汉市江夏区汤逊湖北路38号光谷总部空间
出版文献量(篇)
426
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0
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