brightness temperature
3.5. Computing the regression coefficients with AIRS brightness temperature and thecorresponding T213 temperature analyses field make for AIRS operational retrieval.
4.Collocated AIRS brightness temperature and the corresponding T213 temperatureanalyses field are used to compute the regression coefficients.
5.DETERMINATION OF THE SOLAR RADIO BRIGHTNESS TEMPERATURE DISTRIBUTION AT 8.6MM WAVELENGTH BASED ON THE OBSERVATIONS OF THE ANNULAR SOLAR ECLIPSE
6.the relationship between the linear combination of NDVI and brightness temperature of 31 band (T31) was significantly high in the region of high vegetation cover, and so did T31/NDVI, the performance of EVI and SAVI was not satisfactory;
7.The temperature and humidity profiles from operational TO VS data, as well as some others data necessary to run RTTOV5, are used to comput e the brightness temperature with respect to HIRS channels in NOAA14. Then the i mpact of the cloud fraction and the top of cloud on simulated errors in models a re estimated.
8.Based on cloud-top brightness temperature data and circulation background, and the physical quantities, Diagnosis of severe convection weather caused by MCS in Mei-yii front over the Yellow Sea-Changjiang River during June 21 to 23, 2002 is made.
9.The AIRS cloud-cleared radiance spectrum is spectrally reduced to mimic all MODISinfrared spectral bands within the AIRS spectral range. These aggregated measurements, MODIS-like in spectral coverage but at the spatial resolution of AIRS, are expressed as brightness temperatures and are compared with MODIS clear sky brightness temperature observations within all successfully cloud-cleared AIRS footprints.
10.In this paper,the microwave brightness temperature(MBT) data from TRMM/TMI and the precipitation rate from TRMM/PR were used in the precipitation retrieval of typhoon Aere(2004),for three periods during it approaches Taiwan island. Four schemes were conducted in the precipitation retrieval,respectively.
