Smith W L, Zhou F X
NOAA National Earth Satellite Service, Madison, Wisconsin 53706, USA.
Appl Opt. 1982 Mar 1;21(5):924-8. doi: 10.1364/AO.21.000924.
Layer moisture and temperature are important variables for forecasting local weather phenomena. The purpose of ths paper is to present a method to rapidly compute layer average relative humidities and geopotential thicknesses from satellite measurements of atmospheric water vapor and oxygen radiation emission to space. Both polar-orbiting and geostationary satellite data are considered. Analyses show that the relative humidity and geopotential thickness patterns from satellite data are consistent with radiosonde data. The relative humidity calculation is insensitive to the assumed temperature profile condition. It is shown that time variations of the atmospheric moisture can be monitored from a GOES-4 VAS sequential image. Also an attempt is made to derive the atmospheric stability index, total-totals, by use of satellite derived relative humidities and geopotential thicknesses. The results show good correspondence between the derived stability patterns and subsequent convective weather.
气层湿度和温度是预测局地天气现象的重要变量。本文的目的是提出一种方法,可根据大气水汽和向太空发射的氧辐射的卫星测量数据快速计算气层平均相对湿度和位势厚度。文中考虑了极轨卫星和地球静止卫星数据。分析表明,卫星数据得出的相对湿度和位势厚度模式与无线电探空仪数据一致。相对湿度计算对假定的温度廓线条件不敏感。结果表明,利用GOES - 4甚高分辨率扫描辐射计(VAS)序列图像可以监测大气湿度的时间变化。此外,还尝试利用卫星得出的相对湿度和位势厚度推导大气稳定度指标——总指数。结果表明,推导得出的稳定度模式与随后的对流天气之间具有良好的对应关系。