Estimates of the precision of GPS radio occultations from the COSMIC/FORMOSAT‐3 mission

[1] The Constellation Observing System for Meteorology Ionosphere and Climate (COSMIC)/Formosa Satellite 3 (FORMOSAT-3) is a six-satellite radio occultation mission that was launched in mid-April, 2006. The close proximity of the COSMIC satellites provides a unique opportunity to estimate the precision of the radio occultation remote sensing technique from closely collocated occultations (<10 km separation of tangent points). The RMS difference of refractivity between 10 and 20 km altitude is less than 0.2%, which is approximately twice better than previous estimates obtained from CHAMP and SAC-C collocated occultations, apparently, due to smaller separation of the occultation pairs and due to parallel occultation planes. In the lower troposphere, the maximal RMS is ∼0.8% at 2 km altitude and decreases abruptly to ∼0.2% between 6 and 8 km altitude. The RMS difference of electron density in the ionosphere between 150 and 500 km altitude for collocated occultations is about 103 cm−3.

[1]  H. H. Benzon,et al.  Full Spectrum Inversion of radio occultation signals , 2003 .

[2]  W. H. Tsai,et al.  Improvement of GPS/MET Ionospheric Profiling and Validation Using the Chung-Li Ionosonde Measurements and the IRI model , 2004 .

[3]  Larry J. Romans,et al.  Ionospheric electron density profiles obtained with the Global Positioning System: Results from the GPS/MET experiment , 1998 .

[4]  Anthony J. Mannucci,et al.  CHAMP and SAC-C atmospheric occultation results and intercomparisons , 2004 .

[5]  J. Schofield,et al.  Observing Earth's atmosphere with radio occultation measurements using the Global Positioning System , 1997 .

[6]  Ying-Hwa Kuo,et al.  Monitoring the atmospheric boundary layer by GPS radio occultation signals recorded in the open‐loop mode , 2006 .

[7]  T. P. Yunck,et al.  The role of GPS in precise Earth observation , 1988, IEEE PLANS '88.,Position Location and Navigation Symposium, Record. 'Navigation into the 21st Century'..

[8]  Jaume Sanz,et al.  Improving the Abel inversion by adding ground GPS data to LEO radio occultations in ionospheric sounding , 2000 .

[9]  Christian Rocken,et al.  Inversion and error estimation of GPS radio occultation Data , 2004 .

[10]  X. Zou,et al.  Analysis and validation of GPS/MET data in the neutral atmosphere , 1997 .

[11]  Steven Businger,et al.  GPS Sounding of the Atmosphere from Low Earth Orbit: Preliminary Results , 1996 .

[12]  L. Grunwaldt,et al.  GPS radio occultation measurements of the ionosphere from CHAMP: Early results , 2002 .

[13]  Christian Rocken,et al.  Analysis and validation of GPS/MET radio occultation data in the ionosphere , 1999 .

[14]  Douglas Hunt,et al.  GPS profiling of the lower troposphere from space: Inversion and demodulation of the open‐loop radio occultation signals , 2006 .

[15]  S. Sokolovskiy Effect of superrefraction on inversions of radio occultation signals in the lower troposphere , 2003 .

[16]  Christian Rocken,et al.  COSMIC System Description , 2000 .

[17]  S. Syndergaard,et al.  Preparing for COSMIC: Inversion and Analysis of Ionospheric Data Products , 2006 .

[18]  M. Gorbunov,et al.  Comparative analysis of radio occultation processing approaches based on Fourier integral operators , 2004 .

[19]  Rolf König,et al.  Atmosphere sounding by GPS radio occultation: First results from CHAMP , 2001 .

[20]  Ying-Hwa Kuo,et al.  Assimilation of GPS radio occultation data for numerical weather prediction , 2000 .

[21]  Xiaoqing Pi,et al.  COSMIC GPS Ionospheric Sensing and Space Weather , 2000 .

[22]  E. Robert Kursinski,et al.  Accuracies of atmospheric profiles obtained from GPS occultations , 1993 .

[23]  W. G. Melbourne,et al.  The application of spaceborne GPS to atmospheric limb sounding and global change monitoring , 1994 .

[24]  W. Bertiger,et al.  A technical description of atmospheric sounding by GPS occultation , 2002 .