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SWAN模式对陆架浅水区有效波高的模拟研究及改进
作者:蒋廷松  任建莉  沈彩琴 
单位:浙江工业大学机械工程学院能源与动力工程研究所, 浙江杭州310014
关键词:SWAN 陆架浅水区 白浪耗散 有效波高 
分类号:731.22
出版年·卷·期(页码):2014·31·第四期(9-17)
摘要:
验证了QSCAT/NCEP混合风场,并将其作为SWAN模式的驱动风场。以南黄海海域作为目标区域,对SWAN模式在陆架浅水区有效波高的模拟能力进行了研究。研究表明,默认参数下SWAN模式计算的有效波高较JASON-1卫星高度计数据偏小,最大偏差达0.6m。通过对SWAN模式中各物理过程的分析,确定模式计算值偏小的原因是白浪耗散过大。采用参数修正法对白浪耗散项进行改进,将SWAN模式计算有效波高的均方根误差降低到0.16m以下,相关系数提高到0.85以上。选择2002年中具有代表性的4个月对改进后SWAN模式进行验证,结果显示SWAN模式在研究区域具有良好的稳定性和适用性。
An assessment of SWAN model in shallow shelf area was performed through the simulation of significant wave height in South Yellow Sea in this paper. The QSCAT/NCEP blended wind field was used to drive the SWAN model. The data of significant wave height calculated by SWAN model with default index were compared with the data extracted from Jason-1 satellite altimeter. Results indicated that the modeled result was smaller than the satellite result, and the maximum deviation was 0.6 meter. By analyzing the main physical process of SWAN model, the reason of data deviation is attributed to higher whitecapping dissipation. The parameters correction method of whitecapping dissipation index was presented, and has been successfully used to improve the SWAN modeling performance in shallow shelf area. The modified simulation result showed that the deviation of significant wave height decreased below 0.16 meters, and the correlation coefficient increased to more than 0.85. Finally, the modified SWAN model was used to calculate the significant wave height for four typical months in 2002. It was found that the simulation results from modified SWAN model were compatible with Jason-1 data. The modified SWAN model is suitable and stable for simulation of significant wave height in Shallow shelf area.
参考文献:
[1] Swan Team. Swan user (40.85A)[R]. Delft: Delft University of Technology, 2008.
[2] 贾晓, Bardur N, 潘军宁, 等. SWAN模型风能输入项的改进与验 证[J]. 河海大学学报(自然科学版), 2010, 38(5): 585-591.
[3] Ris R C, Holthuijsen L H, Booij N. A third-generation wave model for coastal regions 2. Verification[J]. Journal of Geophysical Research, 1999, 104(4): 7667-7681.
[4] Gorman R M, Neilson C G. Modeling shallow water wave generation and transformation in an intertidal estuary[J]. Coastal Engineering, 1999, 36(3): 197-217.
[5] Padilla H R, Monbaliu J. Energy balance of wind waves as a function of the bottom friction formulation[J]. Coastal Engineering, 200l, 43(2): 131-148.
[6] Lin W Q, Sanford L P, Suttles S E. Wave measurement and modeling in Chesapeake Bay[J]. Continental Shelf Research, 2002, 22(18-19): 2673-2686.
[7] 徐福敏, 张长宽, 陶建峰, 等. 浅水波浪数值模型SWAN的原理及 应用综述[J]. 水科学进展, 2004, 15(4): 538-542.
[8] 徐艳清, 尹宝树, 杨德周, 等. 东中国海海浪数值模式的研究[J]. 海洋科学, 2005, 29(6): 42-47.
[9] 闫涛, 张宇铭, 胡保全, 等.WAVEWATCH和SWAN嵌套模拟台风 浪场的结果分析[J].海洋湖沼通报, 2009, 4: 1-7.
[10] 王毅. SWAN模式及数据同化技术在海浪预报中的试验研究和 应用[D]. 青岛: 中国海洋大学, 2011.
[11] Zubier K M. Numerical wave simulations on different oceanic scales[D]. Maine: The University of Maine. 2002.
[12] Scientific and technical documentation (40.85)[R]. Delft: Delft University of Technology, 2008.
[13] 李燕, 薄兆海. SWAN模式对黄渤海海域浪高的模拟能力试验
[J]. 海洋预报, 2005, 22(3): 75-82.
[14] 刘博, 甘薇薇, 任凤杰, 等. Jason-1 海洋地形卫星介绍[J]. 贵州气 象, 2011, 35(1): 42-44.
[15] 程永存, 徐青, 刘玉光, 等. T/P, Jason-1 测量风速及有效波高的 验证与比较[J]. 大地测量与地球动力学, 2008, 28(6): 117-122.
[16] PO. DAAC. AVISO and PODAAC User Handbook[K]. IGDR and GDR Jason Products, 2004.
[17] 于振涛. JASON-1 和TOPEX/POSEIDON 卫星高度计数据在中 国海和西北太平洋的校正、印证及数据融合[D]. 青岛: 中国海 洋大学, 2006.
[18] 王道龙. 近岸海浪模式研究[D]. 青岛: 国家海洋局第一海洋研 究所, 2009.
[19] 李靖, 周林, 郑崇伟, 等. 台湾海峡及其邻近海域波浪能资源评 估[A]. 中国可再生能源学会. 中国可再生能源学会2011 年学术 年会论文集[C]. 中国可再生能源学会, 2011: 4.
[20] 张进峰. 典型海域的海浪数值模拟研究[D]. 武汉: 武汉理工大 学, 2005.
[21] Rogers W E, Paul A H, David W W. Investigation of Wave Growth and Decay in the SWAN model: Three Regional-Scale Appljcations[J]. J Phys Oceanogr, 2003, 33: 366-389.
[22] Komen G J, Hasselmann S, HasseJmann K. On the existence of a fully developed wind-sea Spectrum[J]. J Phys Oceanogr, 1984, 14: l27l-l285.
[23] Janssen P A E M. Consequences of the effect of surface gravity waves on the mean air flow[J]. Int Union of Theor and AppI Mech (IUTAM), 1992, 193-198.
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