WAVEWATCH-Ⅲ海浪模式中岛屿次网格效应的检验与比较

毛科峰; 陈希; 李妍; 张韧

WAVEWATCH-Ⅲ海浪模式中岛屿次网格效应的检验与比较

解放军理工大学气象海洋学院, 江苏南京 211101

基金项目: 国家自然科学基金(41075045);卫星海洋环境动力学国家重点实验室开放研究基金(SOED1009)。

计量
- 文章访问数: 1380
- HTML全文浏览量: 9
- PDF下载量: 1085
- 被引次数: 0
出版历程
- 收稿日期: 2011-07-22
- 修回日期: 2012-03-12

Validation and comparison of sub-grid islands effect in ocean wave model of WAVEWATCH-Ⅲ

Institute of Meteorology and Oceanography, PLA University of Science and Technology, Nanjing 211101, China

摘要

摘要: 综合利用水深数据和高分辨率海岸线数据,在优化WAVEWATCH-Ⅲ模式计算网格的基础上,发展了波能通量穿透度系数自动计算方法,完善了岛屿次网格地形效应计算方案;并与直接提高网格空间分辨率来分辨多岛屿地形处理方案的计算效果进行对比研究。表明:岛屿次网格效应方案充分体现了海岸和多岛屿地形对海浪传播的影响,且主要是对低频海浪能量的抑制和阻碍作用,对模式计算结果有明显改善;在低分辨计算网格中考虑岛屿次网格效应时,模式对有效波高的计算精度与高分辨率网格的结果精度相当,且计算效率有显著提高。
- WAVEWATCH-Ⅲ模式 /
- 次网格效应 /
- 通量穿透度系数
Abstract: In order to improve the sub-grid effect,a method for automatically computing the energy flux transparency in WAVEWATCH-Ⅲ model has been established basing on the optimization of computing grid by using depth and high resolution coastlines.The results with the improving sub-grid effect are compared with that directly increasing grid resolution to identify out islands.It shows that the improving sub-grid effect could adequately describe the effect of multi-islands and complex terrain on wave spreading by restraining low-frequency wave energy and the simulation results are well improved.By improving sub-grid effect in low resolution grid,the calculation efficiency is highly increased and the accuracy of significant wave height is equivalent with the results using high resolution grid.
- WAVEWATCH-Ⅲ model /
- sub-grid effect /
- the energy flux transparency

HTML全文

参考文献(11)

WAMDI Group.The WAM model-A third generation ocean wave prediction model[J].J Phys Oceanography,1988,18(8):1775-1810.

Holthuijsen L H.SWAN III version 40.45 USER MANUAL.Delft of Netherlands: Delft University of Technology,2006.

TOLMAN H L.User manual and system documentation of WAVEWATCH-Ⅲ version 2.22.NOAA/NWS/NCEP/MMAB Technical Note,2002-12-18.

TOLMAN H L.Alleviating the garden sprinkler effect in wind wave models[J].Ocean Modelling,2002,4(3):269-289.

HARDY T A,MASON L B,McCONOCHIE J D.A wave model for the Great Barrier Reef[J].Ocean Engineering,2001,28:45-70.

HENDRIK L T.Treatment of unresolved islands and ice in wind wave models[J].Ocean Modelling,2003,5(3):219-231.

U.S.Department of Commerce,National Oceanic and Atmospheric Administration,National Geophysical Data Center,2006.2-minute Gridded Global Relief Data (ETOPO2v2).http://www.ngdc.noaa.gov/mgg/fliers/06mgg01.html

FEITO F R,TOMES J C,URENA L A.Orientation simplicity and inclusion test for planar polygons[J].Com-puter & Graphics,1995,19(4):595-600.

LEONARD B P.A stable and accurate convective modeling procedure based on quadratic upstream interpolation[J].Comput Methods Appl Mech Engng,1979,19(1):59-98.

HOLLAND G J.An Analytic model of the wind and pressure profiles in Hurricanes[J].Mon Wea Rev,1980,108(8):1212-1215.

YUEH S H,STILES B W,TSAI W Y,et a1.QuikSCAT geophysical model function for tropical cyclones and application to hurricane Floyd[J].Geoscience and Remote Sensing,2001,39:2601-2612.

施引文献

资源附件(0)

访问统计