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海南岛地形对局地海风环流结构影响的数值模拟

杨秋彦 苗峻峰 王语卉

杨秋彦, 苗峻峰, 王语卉. 海南岛地形对局地海风环流结构影响的数值模拟[J]. 海洋学报, 2017, 39(3): 24-43.
引用本文: 杨秋彦, 苗峻峰, 王语卉. 海南岛地形对局地海风环流结构影响的数值模拟[J]. 海洋学报, 2017, 39(3): 24-43.
Yang Qiuyan, Miao Junfeng, Wang Yuhui. A numerical study of impact of topography on sea breeze circulation over the Hainan Island[J]. Haiyang Xuebao, 2017, 39(3): 24-43.
Citation: Yang Qiuyan, Miao Junfeng, Wang Yuhui. A numerical study of impact of topography on sea breeze circulation over the Hainan Island[J]. Haiyang Xuebao, 2017, 39(3): 24-43.

海南岛地形对局地海风环流结构影响的数值模拟

基金项目: 公益性行业(气象)科研专项经费项目(GYHY201306009)。

A numerical study of impact of topography on sea breeze circulation over the Hainan Island

  • 摘要: 本文利用WRF模式对2014年5月25日发生在海南的一次海风过程进行了数值模拟,通过地形敏感性试验,探讨了海南岛地形对局地海风环流结构的影响。结果表明:控制试验(CNTL)海风于15时左右达到强盛。无地形试验(FLAT)中,水平方向上,海风持续时间缩短,南、北、西向海风向内陆传播距离变短1~5 km,海风强度减弱1 m/s左右,海风动能及辐合强度在沿海地区及西南山区存在大值衰减区;垂直方向上,海风碰撞位置向西、北方向移动,高空回流高度降低,海风厚度减小,垂直环流强度减弱2~6 m2/s2,海风锋附近的垂直速度减小10 cm/s以上。谷风对海风同相叠加作用的消失也使得海风强度减弱。其主要影响机制为:在动力方面,由山脉屏障作用引起的海风强迫抬升、绕流等增强作用消失;在热力方面,地表吸收净辐射减少,导致其向大气中释放的感热、潜热通量等各项均减少约9%,这种改变造成了海陆之间温度、气压差的减小,最终造成了海风的减弱。此外,通过两组削山试验,发现海拔高度降低区辐合范围、强度及动能均减小,同时海风垂直环流结构也相应发生改变,其中移去黎母山脉(RMLM)对海风环流结构的影响大于移去五指山脉(RMWZ)。
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  • 收稿日期:  2016-05-22

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