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Absorption and scattering of 1.06 (mu)m laser radiation from oceanic aerosols

机译:1.06μm激光辐射从海洋气溶胶中的吸收和散射

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摘要

The absorption and scattering of oceanic aerosols are characterized using low- and high-power lasers in the near IR (1.064 (mu)m). The imaginary part of the refractive index of sea salt inferred from low-power absorption measurements is 200x less than the commonly accepted value from the literature. The measured absorption coefficients of natural and artificial saltwater are within 5percent of the absorption of pure water (0.14 cm~(-1)). High-power aerosol experiments are consistent with low-power liquid absorption measurements, which yield comparable absorption coefficients for pure water and saltwater. High-power illumination of test aerosols (CuSO_(4) (centre dot) 5H_(2)O) with an absorption coefficient alpha >= 0.19 cm~(-1) and a dwell time of 100 ms results in a consistent reduction in scattering from the aerosol column. The high-power laser scattering measurements are in good agreement with the theory, which accounts for the absorption, heating, and vaporization of the water-based aerosols. The measured absorption of oceanic aerosols in the laboratory is much less than the literature values at 1.064 (mu)m and should result in reduced heating and thermal blooming in open ocean atmospheres.
机译:使用近红外(1.064μm)中的低功率和高功率激光来表征海洋气溶胶的吸收和散射。从低功率吸收测量得出的海盐折射率的虚部比文献中公认的值小200倍。测得的天然和人造盐水的吸收系数在纯水(0.14 cm〜(-1))的5%之内。高功率气溶胶实验与低功率液体吸收测量结果一致,后者得出的纯水和盐水吸收系数相当。吸收系数alpha> = 0.19 cm〜(-1),停留时间为100 ms的测试气雾剂(CuSO_(4)(中心点)5H_(2)O)的大功率照明导致散射持续降低从气溶胶柱。高功率激光散射测量与理论相吻合,该理论考虑了水基气溶胶的吸收,加热和汽化。在实验室中测得的海洋气溶胶吸收率远小于文献中1.064μm的吸收值,这将导致在开放的海洋大气层中减少的热量和热量散发。

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