首页> 外文期刊>Journal of Geophysical Research, C. Oceans: JGR >Nonlinear and minor ocean tides in the Bay of Biscay from the strain tides observed by two geodetic laser strainmeters at Canfranc (Spain)
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Nonlinear and minor ocean tides in the Bay of Biscay from the strain tides observed by two geodetic laser strainmeters at Canfranc (Spain)

机译:比斯开湾的非线性和次要海洋潮汐,由坎弗兰克(西班牙)的两个大地测量激光应变仪观测到的应变潮

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This work presents and discusses the tidal analysis of about 2.5 years of strain data recorded by two 70 m-long high-resolution laser strainmeters, which are operating in the Canfranc underground laboratory (Central Pyrenees, Spain). Spectra show clear tidal peaks whose frequencies range from the diurnal band to at least 8 cycles per day; strain amplitudes (relative change in length for each strainmeter) range from few 10~(-12) to 10~(-8). The reliability of observations and corrections for local distortions are testified by the excellent agreement between measurements and computations for all the diurnal and semidiurnal tides included in the TPXO8 and FES2012 tidal atlases, with the exception of L2. Observed higher-frequency strain tides are mostly attributed to loading by nonlinear shallow-water constituents in the Bay of Biscay, more than 120 km from the measurement site. The signals are quantitatively compared with computations using TPXO8 (MN4, M4, and MS4) and FES2012 (M3, N4, MN4, M4, MS4, and M6). Computations fully agree with M4 observations for one strainmeter, overestimate M4 by about 30% for the other strainmeter and M6 by about a factor of two, and underestimate the other tides. This work shows that data from high-sensitivity strainmeters installed in high-quality sites may provide valuable additional information for studying the nonlinear tidal dynamics and energetics of coastal waters and minor ocean tides, at spatial resolutions of tens to thousands square kilometers, depending on the strainmeter location with respect to the coastline.
机译:这项工作介绍并讨论了由两台70 m长的高分辨率激光应变仪记录的大约2.5年的应变数据的潮汐分析,这两个应变仪在Canfranc地下实验室(西班牙中比利牛斯山脉)中运行。频谱显示清晰的潮汐峰,其频率范围从昼夜波段到每天至少8个周期。应变幅度(每个应变仪的长度相对变化)范围从10〜(-12)到10〜(-8)。对于TPXO8和FES2012潮汐图册中除L2以外的所有日潮和半日潮,测量和计算之间的出色一致性证明了观测和校正局部变形的可靠性。观测到的高频应变潮主要归因于比斯开湾的非线性浅水成分所造成的负荷,该区域距测量地点超过120公里。将信号与使用TPXO8(MN4,M4和MS4)和FES2012(M3,N4,MN4,M4,MS4和M6)的计算进行定量比较。计算完全符合一个应变仪的M4观测值,另一个应变仪的M4估算值高估约30%,M6的M6估算值约高2倍,而其他潮流计则低估。这项工作表明,安装在高质量站点的高灵敏度应变仪的数据可能为研究沿海水域和小潮汐的非线性潮汐动力学和能量学提供有用的附加信息,空间分辨率为数十到数千平方公里,具体取决于应变仪相对于海岸线的位置。

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