设为首页
加入收藏
一次冷锋过境后的海风三维结构数值模拟
Numerical Simulation of a Sea Breeze Event After the Passage of a Cold Front
-
摘要: 为研究大尺度系统风对海风的影响以及海风三维结构特征，利用山东省123个地面自动站资料、青岛地区三十多个内陆及沿海、海岛观测站以及奥帆赛场3个浮标站资料，对2006年8月21日青岛一次海风个例进行了分析，并利用美国俄克拉荷马大学风暴分析预测中心开发的ARPS（the Advanced Regional Prediction System）模式，对海风过程进行了数值模拟研究。结果发现：在较强的离岸风背景下，当内陆气温高于海面气温2 ℃ 左右时，海风也可以发生。海风首先在海岸线附近的海上开始，发展的同时向内陆及远海地区推进。海风低层环流很浅，主要位于500 m 以下。在较强的偏北离岸风下，海风向内陆推进的距离很短。偏北的大尺度系统风由于渤海冷下垫面的影响，不利于青岛海风的维持。海风开始时，在1500～2500 m 高度处同时有反环流出现，但直到傍晚前后，海风的垂直环流圈才发展得比较清晰，其高度也更接近地面。海风消亡后，高层的垂直环流圈及反环流维持3 h 左右才逐渐消亡。Abstract: A sea breeze event occurs on 21 August 2006 when a cold front passes Shandong Province and the synoptic scale wind is northerly. In order to analyze the development of the sea breeze, the feature of the sea breeze is analyzed with 123 AWS data in Shandong Province, over 30 AWS station data in Qingdao area, in the island and three buoys in the sailing spots. As a result, the detailed AWS station data in the coastal area and buoys can give more detailed and new feature of the sea breeze. Further more, these data are assimilated into the ARPS (the Advanced Regional Prediction System) model. The controlled experiment uses 2 level 1 way nested grids, with the horizontal resolutions of 30 km and 6 km respectively. In vertical, a scheme consisting of 53 sigma z levels with a minimum thickness layer of about 20 m near the surface and vertically stretched grids extending to model tops at about 20 km height is used. Compared with the observation, the model can simulate development of the sea breeze reasonably. With the observation and the simulation, the detailed feature of the boundary wind and 3 dimension structure of the sea breeze are analyzed, indicating that the sea land temperature difference of around 2 ℃ causes the sea breeze in this case. Under the northerly wind, the surface temperature to the south of Qingdao rises faster than that on the north land, thus the sea breeze mainly occurs in the southeast coastal region. The sea breeze begins offshore and then develops into the land and the far ocean widely. The vertical height of the sea breeze circulation is as shallow as below 500 m. Due to the stronger offshore synoptic scale wind the sea breeze can only spread to very limited area along the coastal line. The northerly synoptic wind passes over the Bohai Sea and causes cold surge to land in Shandong Province, which is adverse for the sea breeze maintaining, as a result, the sea breeze in the southeast coastal region of Shandong Province dies earlier at around 17:00. When the sea breeze begins the reverse circulation forms around 1500—2500 m height at the same time. But the vertical circulation doesn't develop clearly until the evening and the height of it is below 1000 m. The vertical circulation and the reverse circulation can last 3 hours after the sea breeze dies.
-
Key words:
- sea breeze;
- formation feature;
- numerical simulation;
- 3 dimension structure
-
图 1 2006年8月21日青岛奥帆赛场附近3个浮标站以及青岛站风速 (a)、风向 (b) 演变曲线 (浮标B在15：00风速以前缺测) 以及08：00(c) 和17：00(d) 山东省123个地面自动站观测的风场
Fig. 1 Wind speed (a) and wind direction (b) at three buoystation sand Qingdao Station (wind speedatbuoy Bbefore 15:00 is missing) with the wind field at 08:00 (c) and 17:00 (d) by the 123 AWS in Shandong Provinceon 21 August 2006
图 2 2006年8月21日青岛地区内陆、海岛自动站及浮标站观测的风场演变 (图中红色数字为气温，单位：℃)
Fig. 2 Surface wind field from the AWS in land and is land, and buoys in Qingdao on 21 August 2006 (red numbers denote air temperature, unit:℃)
图 3 2006年8月21日模式6km网格模拟的近地面10m风场 (矢量，单位：m·s-1) 和温度场 (绿线，单位：℃)(阴影部分为地形高度)(a)08：00，(b)11：00，(c)14：00，(d)17：00
Fig. 3 Surface wind field (vector, unit:m·s-1) and temperature (greenline, unit:℃) simulated by the 6-km grid on 21 August 2006 (shadow areas are altitude terrain)(a)08:00, (b)11:00, (c)14:00, (d)17:00
图 4 模式6km网格模拟的2006年8月21日青岛站以及浮标站风速 (a)、风向 (b)、地面气温 (c) 的演变以及地面气温实况 (d)(浮标A与B的风速、风向与气温模拟结果重合)
Fig. 4 Simulated wind speed (a), wind direction (b), surface air temperature (c) for buoys and Qingdao Station at 6-km grid and the temperature observations (d) on 21 August 2006 (the simulated wind and temperature at buoy A and Bisthe same)
图 5 模式6km网格模拟的2006年8月21日08：00(a) 和17：00(b) u-v风场和气温场以及13：00(c)、18：00(d) u-w风场矢量、气温 (点划线，单位：℃) 和垂直速度 (实线，单位：m·s-1) 沿36°N的垂直剖面 (其中，w放大了25倍)
Fig. 5 Simulated cross-section of wind and temperature at 08: 00 (a), 17: 00 (b) and w-w wind (vector, mis multiplied 25), temperature (dotted-dashed line, unit: ℃) and w component (solid line, m • s-1) along 36°N at 13 :00 (c) and 18 :00 (d) by 6-km grid on 21 August 2006
-
[1] Bethwaite F,High Performance Sailing,International Marine,Grest Britain,1993:1-414. [2] Alain C,Msrtilli A,Grossi P,Effect of sea breeze on air pollution in the Greater Athens Area.Part I;Numerical simulations and field observations,Journal of Applied Meteorology,2000,39:546-562. [3] Haurwitz B,Comments on "The sea-breeze circulation",J Mete-or,1947,27:675-679. [4] Defant A,Local Winds,Amer Mereor Soc,1951:658-672. [5] Estoque M A,A theoretical investigation of the sea breeze,Quarterly Journal of the Royal Meteorological Society,1961,17:645-660. http://cn.bing.com/academic/profile?id=705ab601c4dde7cd38fc7b87a964f4b1&encoded=0&v=paper_preview&mkt=zh-cn [6] Houghton D,Campbell F,Wind Strategy.Fernhurst Books,England,2005:1-128. [7] 吴增茂,龙宝森.青岛局地风特征的分析.海洋湖沼通报,1993(1):16-21. http://www.cnki.com.cn/Article/CJFDTOTAL-HYFB199301002.htm [8] 庄子善,郑美琴,王继秀,等.日照沿海海陆风的气候特点及其对天气的影响.气象,2005,31(9):66-70. http://www.cnki.com.cn/Article/CJFDTOTAL-QXXX200509013.htm [9] 薛德强,郑全岭,钱喜镇,等.龙口的海风及其影响.海洋湖沼通报,1995(2):1-9. http://www.cnki.com.cn/Article/CJFDTOTAL-HYFB199503000.htm [10] 薛德强,郑全岭,钱喜镇,等.山东半岛的海陆风环流及其影响.南京气象学院学报,1995,18(2):293-299. http://www.cnki.com.cn/Article/CJFDTOTAL-NJQX502.020.htm [11] 盛春岩,王建林,刁秀广.2006年8月青岛国际帆船赛期间海陆风特征及三维结构分析.中国海洋大学学报(自然科学版),2007,37(4):609-614. http://www.cnki.com.cn/Article/CJFDTOTAL-QDHY200704018.htm [12] Sheng C Y,Xue M,Gao S T,The structure and evolution of sea breezes during the Qingdao Olympic sailing test event in 2006,Advances in Atmospheric Sciences,2009,26:132-142. doi: 10.1007/s00376-009-0132-y [13] 高荣珍,林行,孙贞.青岛近海夏季海风特征及其预报方法研究.中国海洋大学学报(自然科学版),2008,38(5):699-704. http://www.cnki.com.cn/Article/CJFDTOTAL-QDHY200805004.htm [14] 李明华,范绍佳,王宝民,等.珠江三角洲秋季大气边界层温度和风廓线观测研究.应用气象学报,2008,19(1):53-60. http://qikan.camscma.cn/jams/ch/reader/view_abstract.aspx?file_no=20080110&flag=1 [15] 付秀华,李兴生,吕乃平,等.复杂地形条件下三维海陆风数值模拟.应用气象学报,1991,2(2):113-123. http://qikan.camscma.cn/jams/ch/reader/view_abstract.aspx?file_no=19910217&flag=1 [16] 苗世光,孙桂平,马艳,等.青岛奥帆赛高分辨率数值模式系统研制与应用.应用气象学报,2009,20(3):370-379. http://qikan.camscma.cn/jams/ch/reader/view_abstract.aspx?file_no=20090315&flag=1 [17] Xue M,Droegemeier K K,Wong V,ARPS Version 4.0 User's Guide,Center for Analysis and Prediction of Storms,University of Oklahoma,1995:1-380. [18] Xne M,Droegemeier K K,Wong V,The Advanced Regional Prediction System(ARPS)-A multi-scale nonhydrostatic at-mospheric simulation and prediction model.Part I:Model dynamics and verification,Meteorology and Atmospheric Physics,2000,75:161-193. [19] Xue M,Droegemeier K K,Wong V,The Advanced Re-gioml Prediction System(ARPS)-A multi-scale nonhydrostatic atmospheric simuhtion and prediction model Part Ⅱ:Model physics and applications,Meteorology and Atmospheric Physics,2001,76:143-165. doi: 10.1007/s007030170027 -
下载:
计量
- 摘要浏览量: 4212
- HTML全文浏览量: 852
- PDF下载量: 1473
- 被引次数: 0
