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Estimates of the precision of GPS radio occultation bending angles in the neutral atmosphere from the COSMIC/ FORMOSAT-3 Mission [presentation]
Follow-on radio occultation constellations for meteorology, ionosphere and climate: Overview of currently planned missions, data quality and coverage, and potential science applications [presentation]
Data assimilation retrieval of electron density profiles from radio occultation measurements [presentation]
Structural uncertainty of the CHAMP climate record from different data centers [presentation]
Using SI-traceable global positioning system radio occultation measurements for climate monitoring [In "State of the Climate in 2009"]
Global evaluation of radiosonde water vapor systematic biases using GPS radio occultation from COSMIC and ECMWF analysis
Climatology of ionospheric upper transition height derived from COSMIC satellites during the solar minimum of 2008
Global ionospheric response observed by COSMIC satellites during the January 2009 SSW [presentation]
Global ionospheric response observed by COSMIC satellites during the January 2009 stratospheric sudden warming event [poster]
Data assimilation using COSMIC data: Some general ideas [presentation]
Artificial plasma cave in the low-latitude ionosphere results from the radio occultation inversion of the FORMOSAT-3/COSMIC
Development of a curved ray tracing method for modeling of phase paths from GPS radio occultation: A two-dimensional study
Variability of the boundary layer depth over certain regions of the subtropical ocean from 3 years of COSMIC data [presentation]
GPS TEC response to the 22 July 2009 total solar eclipse in East Asia
COSMIC GPS radio occultation temperature profiles in clouds
Impact of FORMOSAT-3/COSMIC GPS radio occultation and dropwindsonde data on regional model predictions during the 2007 Mei-yu season
GPS multipath and its relation to near-surface soil moisture content
The beneficial impact of radio occultation observations on Australian region forecasts
A physical model for GPS multipath caused by land reflections: Toward bare soil moisture retrievals

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