TY - GEN
T1 - Microwave radiative transfer at frequencies of AMSU-B
T2 - 2009 IEEE International Geoscience and Remote Sensing Symposium, IGARSS 2009
AU - Xie, Xinxin
AU - Miao, Jungang
AU - Wang, Wei
PY - 2009
Y1 - 2009
N2 - This paper presents the effects of uncertainties in ice permittivity on emerging brightness temperatures at three different zenith angles at the frequencies of Advanced Microwave Sounding Unit-B (AMSU-B), 89 GHz, 150 GHz and 183 GHz. The absolute error of brightness temperature, due to an uncertainty of ±20% in the imaginary part of ice permittivity and of ±5% in the real part, is explored with vector discrete ordinate radiative transfer (VDISORT) method at the zenith angle of 0°, 30° and 53° in this study. Particles in clouds are taken to be spheres, of which the diameters are uniformly distributed in the range of 40 μm to 4000 μm in Gamma-size distribution. We found that ±5% uncertainty in the real part of ice permittivity results in more than 1 K variation in upwelling brightness temperature, higher than ±20% uncertainty in the imaginary part when the effective diameter in Gamma-size distribution is 150 μm. And the absolute error of brightness temperature caused by uncertainties in ice permittivity is up to more than 2 K at the zenith angle of 53°, greater than the corresponding value at the other two zenith angles.
AB - This paper presents the effects of uncertainties in ice permittivity on emerging brightness temperatures at three different zenith angles at the frequencies of Advanced Microwave Sounding Unit-B (AMSU-B), 89 GHz, 150 GHz and 183 GHz. The absolute error of brightness temperature, due to an uncertainty of ±20% in the imaginary part of ice permittivity and of ±5% in the real part, is explored with vector discrete ordinate radiative transfer (VDISORT) method at the zenith angle of 0°, 30° and 53° in this study. Particles in clouds are taken to be spheres, of which the diameters are uniformly distributed in the range of 40 μm to 4000 μm in Gamma-size distribution. We found that ±5% uncertainty in the real part of ice permittivity results in more than 1 K variation in upwelling brightness temperature, higher than ±20% uncertainty in the imaginary part when the effective diameter in Gamma-size distribution is 150 μm. And the absolute error of brightness temperature caused by uncertainties in ice permittivity is up to more than 2 K at the zenith angle of 53°, greater than the corresponding value at the other two zenith angles.
KW - Brightness temperature
KW - Microwave radiative transfer
KW - Uncertainties in ice permittivity
UR - https://www.scopus.com/pages/publications/77951130191
U2 - 10.1109/IGARSS.2009.5418188
DO - 10.1109/IGARSS.2009.5418188
M3 - 会议稿件
AN - SCOPUS:77951130191
SN - 9781424433957
T3 - International Geoscience and Remote Sensing Symposium (IGARSS)
SP - II714-II717
BT - 2009 IEEE International Geoscience and Remote Sensing Symposium, IGARSS 2009 - Proceedings
Y2 - 12 July 2009 through 17 July 2009
ER -