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L-Band Model Function of the Dielectric Constant of Seawater

机译:海水介电常数的L带模型函数

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This paper describes a new model of the seawater dielectric constant as a function of salinity and temperature at L-band. The model function is developed by fitting the accurate measurement data made at 1.413 GHz to a third-order polynomial. The purpose of this study is to provide an accurate model for earth-observing satellites to retrieve seawater salinities from remote sensing data. In this paper, the development of the model function is introduced along with an analysis of the goodness of fit. The model function is then compared with the model functions of Klein-Swift and Meissner-Wentz. Finally, the comparison is made between the retrieved salinity from the satellite data with the in situ data measured by Argo floats.
机译:本文描述了一种新的海水介电常数模型,该模型是L波段盐度和温度的函数。通过将1.413 GHz处的精确测量数据拟合到三阶多项式来开发模型功能。这项研究的目的是为地球观测卫星提供一个准确的模型,以从遥感数据中检索海水盐度。在本文中,介绍了模型功能的开发以及对拟合优度的分析。然后将模型函数与Klein-Swift和Meissner-Wentz的模型函数进行比较。最后,将卫星数据中的盐度与Argo浮子测得的原位数据进行比较。

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