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首页> 外文期刊>Marine Georesources & Geotechnology >Persian gulf and Oman sea tide modeling using satellite altimetry and tide gauge data (TM-IR01)
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Persian gulf and Oman sea tide modeling using satellite altimetry and tide gauge data (TM-IR01)

机译:波斯湾和阿曼海潮建模使用卫星高度测定和潮仪数据(TM-IR01)

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摘要

Satellite altimetry observations and tide gauge data are invaluable tools to diagnose and resolve tidal constituents over the Oceans and Seas. The aim of this study is to introduce a new purely empirical tide model named TM-IR01 in the Persian Gulf, Oman Sea, and North Indian Ocean. The observations of three altimeter sensors including TOPEX/POSIDON, JASON1, and JASON2 and 13 coastal tide gauge (TG) stations are processed and analyzed in this research. First of all, the least square spectral analysis is utilized to recover the significant tide components and consequently the amplitude and phases of the constituents are found during the tide modeling. Finally, the analysis results are interpolated into a grid of 1/4° using the Kriging method. TM-IR01 model is validated by comparing with TG stations and global tide models. It is shown that for main tidal frequencies M2, S2, K1, and 01 the root mean square error (RMSE) between TM-IR01 and TG stations results are 0.372, 0.130, 0.141, and 0.084 m, respectively, and also the RMSE between TM-IR01 and FES2004 models are 0.231, 0.087, 0.027, and 0.042 m, respectively. Validating with FES2012 and Tpxo7.2, the results obtained are close to the above values.
机译:卫星高处理性观测和潮汐仪表数据是诊断和解决海洋上的潮汐组分的宝贵工具。本研究的目的是在波斯湾,阿曼海和北印度洋中引入名为TM-IR01的新纯粹经验潮汐模型。在本研究中处理并分析了三个高度计传感器,包括Topex / Posidon,Jason1和Jason2和13个沿海潮牌(TG)站的三个高度计传感器。首先,利用最小方形光谱分析来恢复显着的潮汐组分,因此在潮汐建模期间发现成分的幅度和阶段。最后,使用Kriging方法将分析结果插入1/4°的网格中。通过与TG站和全球潮汐模型进行比较验证TM-IR01模型。结果表明,对于主潮汐频率M2,S2,K1和01,TM-IR01和TG站之间的根均线误差(RMSE)分别为0.372,0.130,0.141和0.084米,并且在其间的RMSE也是如此TM-IR01和FES2004型号分别为0.231,0.087,0.027和0.042米。使用FES2012和TPXO7.2验证,所获得的结果接近上述值。

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