论文标题

宽范围的prandtl/schmidt数量频谱的外部尺度,用于海洋光学湍流

Outer scale of the wide-range Prandtl/Schmidt number spectrum on beam wander for oceanic optical turbulence

论文作者

Cai, Jian-Dong, Yao, Jin-Ren, Wang, Han-Tao, Zhang, Hua-Jun, Ren, Ming-Yuan, Zhang, Yu

论文摘要

海洋中的光传播受折射率的影响,该折射率与温度,盐度,外尺度等有关。基于Hill的Model 1(H1),已提出了两种海洋折射率谱(ORI)来描述折射率的二阶特征。最近,根据Hill的Model 4(H4)提出了几种ORIS模型,该模型在高波数(粘性 - 排除范围)中具有更好的精度。但是,作为与实际环境有关的关键参数,外部尺度尚未引入任何基于海洋H4的光谱。在本文中,我们将外部尺度参数放入基于H4的频谱中,该频谱适用于宽范围的prandtl/schmidt编号[opt。表达。 20,11111(2019)]。所提出的外部尺度光谱可用于分析有限的外部刻度环境中的波传播,其平均温度和盐度值不同。我们进一步得出了准激光束的光束游荡公式。 Numerical calculations show that the beam wander influenced by outer-scale length $L_{0}$ is more obvious than that influenced by average temperature $\langle T\rangle$, when $L_{0}$ varies from $10 \rm m$ to $100 \rm m$, and $\langle T\rangle$ ranges from $0^{\circ} \rm C$至$ 30^{\ circ} \ rm c $。当盐度波动占上风($ω\ rightarrow 0 $)时,外部尺度的影响会变得较弱。在横梁徘徊的贡献比例中,温度盐耦合项比温度或盐度项的耦合项大得多。

Light propagation in ocean is influenced by the refractive-index which is related to temperature, salinity, outer-scale, etc. Based on Hill's model 1 (H1), two kinds of oceanic refractive-index spectrum (ORIS) have been proposed to describe the second order characteristic of refractive-index. Most recently, several ORIS models were proposed based on Hill's model 4 (H4), which gave a better precision in high wave-numbers (viscous-diffusive range). However, the outer scale, as a key parameter related to practical environment, has not been introduced into any oceanic H4-based spectra. In this paper, we take the outer-scale parameter into an H4-based spectrum which is adapted to the wide-range Prandtl/Schmidt number [Opt. Express. 20, 11111(2019)]. The proposed outer-scaled spectrum could be used in analyzing wave propagation in limited outer-scaled environment with different values of average temperature and salinity. We further derived the beam wander formula of collimated laser beam. Numerical calculations show that the beam wander influenced by outer-scale length $L_{0}$ is more obvious than that influenced by average temperature $\langle T\rangle$, when $L_{0}$ varies from $10 \rm m$ to $100 \rm m$, and $\langle T\rangle$ ranges from $0^{\circ} \rm C$ to $30^{\circ} \rm C$. When salinity fluctuations prevails ($ω\rightarrow 0$), the influence of outer scale becomes weaker. In contribution proportion of beam wander, the temperature-salt coupling term is the much larger than that of temperature or salinity term.

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