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Technical Note: Remote sensing of sea surface salinity using the propagation of low-frequency navigation signals

机译:技术说明:使用低频导航信号的传播遥感海面盐度

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This paper introduces a potential method for the remote sensing of seasurface salinity (SSS) using the measured propagation delay of low-frequencyLoran-C signals transmitted over an all-seawater path between the Syltstation in Germany and an integrated Loran-C/GPS receiver located inHarwich, UK. The overall delay variations in Loran-C surface waves along thepath may be explained by changes in sea surface properties (especially thetemperature and salinity), as well as atmospheric properties that determinethe refractive index of the atmosphere. After removing the atmospheric andsea surface temperature (SST) effects from the measured delay, the residualdelay revealed a temporal variation similar to that of SSS data obtained bythe European Space Agency's Soil Moisture and Ocean Salinity (SMOS)satellite.
机译:本文介绍了一种潜在的海面盐度(SSS)遥感方法,该方法利用测得的低频Loran-C信号在德国Syltstation与位于此处的集成Loran-C / GPS接收机之间的全海水路径传输的传播延迟进行测量在英国哈里奇。沿路径传播的罗兰-C表面波的整体延迟变化可以通过海面特性(尤其是温度和盐度)的变化以及确定大气折射率的大气特性来解释。从测得的延迟中除去大气和海面温度(SST)的影响后,残留延迟显示出与欧洲航天局土壤湿度和海洋盐度(SMOS)卫星获得的SSS数据相似的时间变化。

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