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红海的海陆风:观测、模拟及与区域水汽输送的关系

The Land-Sea Breeze of the Red Sea: Observations, Simulations, and Relationships to Regional Moisture Transport.

作者信息

Davis Shannon R, Farrar J Thomas, Weller Robert A, Jiang Houshuo, Pratt Lawrence J

机构信息

Department of Physical Oceanography Woods Hole Oceanographic Institution Woods Hole MA USA.

Department of Applied Ocean Physics & Engineering Woods Hole Oceanographic Institution Woods Hole MA USA.

出版信息

J Geophys Res Atmos. 2019 Dec 27;124(24):13803-13825. doi: 10.1029/2019JD031007. Epub 2019 Dec 25.

Abstract

Unique in situ observations of atmospheric conditions over the Red Sea and the coastal Arabian Peninsula are examined to study the dynamics and regional impacts of the local land-sea breeze cycle (LSBC). During a 26-month data record spanning 2008-2011, observed LSBC events occurred year-round, frequently exhibiting cross-shore wind velocities in excess of 8 m/s. Observed onshore and offshore features of both the land- and sea-breeze phases of the cycle are presented, and their seasonal modulation is considered. Weather Research and Forecasting climate downscaling simulations and satellite measurements are used to extend the analysis. In the model, the amplitude of the LSBC is significantly larger in the vicinity of the steeper terrain elements encircling the basin, suggesting an enhancement by the associated slope winds. Observed and simulated conditions also reflected distinct gravity-current characteristics of the intrinsic moist marine air mass during both phases of the LSBC. Specifically, the advance and retreat of marine air mass was directly tied to the development of internal boundary layers onshore and offshore throughout the period of study. Convergence in the lateral moisture flux resulting from this air mass ascending the coastal topography (sea-breeze phase) as well as colliding with air masses from the opposing coastline (land-breeze phase) further resulted in cumulous cloud formation and precipitation.

摘要

对红海和阿拉伯半岛沿海地区独特的大气状况实地观测进行了研究,以探讨当地海陆风环流(LSBC)的动力学及其区域影响。在2008年至2011年的26个月数据记录期间,观测到的LSBC事件全年都有发生,经常出现超过8米/秒的跨岸风速。文中展示了该环流中陆风和海风阶段观测到的向岸风和离岸风特征,并考虑了它们的季节调制。利用天气研究和预报气候降尺度模拟以及卫星测量来拓展分析。在模型中,环绕盆地的较陡峭地形要素附近的LSBC振幅明显更大,这表明相关的坡风起到了增强作用。观测和模拟的状况还反映出LSBC两个阶段中固有潮湿海洋气团明显的重力流特征。具体而言,在整个研究期间,海洋气团的推进和后退与向岸和离岸内边界层的发展直接相关。这种气团沿沿海地形上升(海风阶段)以及与来自相反海岸线的气团碰撞(陆风阶段)导致的侧向水汽通量汇聚,进一步导致了积云形成和降水。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/5ace/7043373/0a09873ed658/JGRD-124-13803-g001.jpg

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