扫描低频微波辐射计的校正

A. Prytz, M. Heron, D. Burrage, M. Goodberlet
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引用次数: 8

摘要

扫描低频辐射计(SLFMR)是一个窄带(24 MHz)辐射计,工作频率为1.413 GHz。它使用一个迪克切换的参考负载和一个空传感器来匹配噪声温度和目标的亮度温度。巴特勒矩阵用于引导8 /spl × / 8相控阵天线进入8个波束方向。当仪器在待绘制的区域上空飞行时,需要校准仪器以获得海面盐度估计。海面温度、海况、波束入射角和气流下坡亮温影响仪表读数。还必须考虑从海面反射到仪器中的太阳和银河辐射的影响。本文的重点是仪器校准,需要考虑仪器内关键位置的传感器测量的各种温度的影响。SLFMR的校准是由Prosensing公司在交付前完成的,但很明显,每次飞行都需要重新校准。讨论了仪器的长期稳定性和根据制造商建议的适当校准参数。这些是由温度的微小变化引起的二阶修正,整个机柜有一个反馈控制回路,将机柜温度保持在标称的40/spl度/C。采用多元线性方法校准仪器,以获得与温度测量相关的一组系数。对所有光束位置的系数进行了评估,并在SLFMR指向上方扫描已知的太阳、月亮和星系中心时进行了检查。在保持目标温度不变的房间里进行进一步的计算。这些校准程序消除了不同波束位置响应之间的不平衡。在澳大利亚东北部的大堡礁泻湖制作的一些早期盐度图证明了这一程序的成功。
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Calibration of scanning low frequency microwave radiometer
The scanning low frequency radiometer (SLFMR) is a narrow-band (24 MHz) radiometer operating at 1.413 GHz. It uses a Dicke-switched reference load and a null sensor to match a noise temperature to the brightness temperature of a target. A Butler matrix is used to steer an 8 /spl times/ 8 phased array antenna into eight beam directions. Calibration is required to obtain sea surface salinity estimates from the instrument as it is flown over an area to be mapped. Sea surface temperature, sea state, beam incidence angle and downwelling brightness temperature of the air affect the instrument readings. Consideration must also be given to the effect of solar and galactic radiation reflected off the sea surface into the instrument. This paper focuses on instrument calibrations which are needed to account for the effects of various temperatures measured by sensors at key locations within the instrument. Calibration of the SLFMR was performed by Prosensing before delivery, but it became clear that re-calibration was necessary for each flying campaign. Long-term stability of the instrument and appropriate calibration parameters in light of those suggested by the manufacturer are discussed. These are second-order corrections which arise from small variations in temperature $the whole cabinet has a feedback control loop to hold the cabinet temperature at a nominal 40/spl deg/C. A multivariate linear approach is used to calibrate the instrument for a set of coefficients associated with the temperature measurements. Coefficients were evaluated for all beam positions and checks were made with the SLFMR pointing upwards to scan across known sources of the sun, moon and the centre of the galaxy. Further calculations were made in a room where the target temperature was kept constant. These calibration procedures removed imbalances between the responses at different beam positions. Success of the procedure is demonstrated with some early salinity maps made in the Great Barrier Reef Lagoon in north-east Australia.
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