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The emissivity of foam-covered water surface at L-band: theoretical modeling and experimental results from the FROG 2003 field experiment

机译:L波段泡沫覆盖水面的发射率:FROG 2003现场实验的理论建模和实验结果

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摘要

Sea surface salinity can be measured by microwave\udradiometry at L-band (1400–1427 MHz). This frequency is a\udcompromise between sensitivity to the salinity, small atmospheric\udperturbation, and reasonable pixel resolution. The description\udof the ocean emission depends on two main factors: 1) the sea\udwater permittivity, which is a function of salinity, temperature,\udand frequency, and 2) the sea surface state, which depends on the\udwind-induced wave spectrum, swell, and rain-induced roughness\udspectrum, and by the foam coverage and its emissivity. This study\udpresents a simplified two-layer emission model for foam-covered\udwater and the results of a controlled experiment to measure the\udfoam emissivity as a function of salinity, foam thickness, incidence\udangle, and polarization. Experimental results are presented, and\udthen compared to the two-layer foam emission model with the\udmeasured foam parameters used as input model parameters. At\ud37 psu salt water the foam-induced emissivity increase is 0.007\udper millimeter of foam thickness (extrapolated to nadir), increasing\udwith increasing incidence angles at vertical polarization,\udand decreasing with
机译:可以通过微波/辐射法在L波段(1400–1427 MHz)测量海面盐度。该频率在对盐度的敏感性,较小的大气/摄动和合理的像素分辨率之间是不妥协的。对海洋排放的描述取决于两个主要因素:1)海水/海水的介电常数,它是盐度,温度,紫外线/频率的函数,以及2)海面状态,其取决于\随风诱导的波谱,膨胀和雨水引起的粗糙度\超谱,以及泡沫覆盖率及其发射率。这项研究提供了一个简化的泡沫覆盖的\ u200b \ u200b两层排放模型,以及一个控制实验的结果,该测量结果是测量\ u泡沫的发射率随盐度,泡沫厚度,入射角\ udangle和极化的函数。给出了实验结果,然后与将测得的泡沫参数用作输入模型参数的两层泡沫排放模型进行了比较。在\ ud37 psu盐水中,泡沫引起的发射率增加为0.007 \ udmm(泡沫厚度(外推至最低点)),在垂直极化时随着入射角的增加而增加\ ud,随

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