【摘要】：赤道太平洋冷舌模擬偏低且過(guò)于西伸是一個(gè)共性問(wèn)題�；谔卣鞑▍�(shù)化理論,利用美國(guó)國(guó)家環(huán)境預(yù)報(bào)中心(National Centers for Environmental Prediction,NCEP)再分析風(fēng)場(chǎng)驅(qū)動(dòng)海浪模式WAVEWATCHⅢ模擬所得的有效波高、波周期、波長(zhǎng)等海浪要素,計(jì)算出海浪混合作用引起的垂直渦動(dòng)動(dòng)量系數(shù)和熱混合系數(shù),將其引入到SBPOM(Stony Brook Parallel Ocean Model)環(huán)流模式的動(dòng)量控制方程中,由此探究海浪混合作用對(duì)熱帶海洋海表面溫度模擬的影響。初步數(shù)值模擬研究結(jié)果表明,海浪混合作用的考慮,有效地改進(jìn)了環(huán)流模式模擬熱帶海洋海表面溫度偏低和赤道冷舌偏冷且過(guò)于西伸的現(xiàn)象,使得環(huán)流模式對(duì)熱帶海洋的模擬效果更好。
[Abstract]:It is a common problem that the simulation of cold tongue in the equatorial Pacific is low and overstretched westward. Based on the characteristic wave parameterization theory and using (National Centers for Environmental Prediction,NCEP (National Center for Environmental Prediction), the effective wave height, wave period, wave length and other ocean wave elements simulated by wind driven wave model WAVEWATCH 鈪，

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