Search results

(1 - 20 of 20)
Abel ionospheric inversion technique and its error analysis
East-west differences in F-region electron density at midlatitude: Evidence from the Far East region
An ionospheric occultation inversion technique based on epoch difference
Statistic analysis of the ionospheric topside scale height based on COSMIC RO measurements
Some characteristics of lightning activity and radiation source distribution in a squall line over north China
Validate the IRI2007 model by the COSMIC slant TEC data during the extremely solar minimum of 2008
Observing system simulation experiment study on imaging the ionosphere by assimilating observations from ground GNSS, LEO-based radio occultation and ocean reflection, and cross link
Characteristics of global precipitable water in ENSO events revealed by COSMIC measurements
Evaluating the effect of the global ionospheric map on aiding retrieval of radio occultation electron density profiles
Quantification of structural uncertainty in climate data records from GPS radio occultation
Improving ensemble-based quantitative precipitation forecasts for topography-enhanced typhoon heavy rainfall over Taiwan with a modified probability-matching technique
Influence of the El Niño Southern Oscillation on the middle and upper atmosphere
The influence of atmospheric tide and planetary wave variability during sudden stratosphere warmings on the low latitude ionosphere
Global variation of COSMIC precipitable water over land: Comparisons with ground-based GPS measurements and NCEP reanalyses
A noise-aware combination of dual-frequency measurements from GPS radio occultation
The effect of solar radio bursts on the GNSS radio occultation signals
GNSS radio occultation (RO) derived electron density quality in high latitude and polar region: NCAR-TIEGCM simulation and real data evaluation
Annual asymmetry in thermospheric density: Observations and simulations
Tropical cyclone cloud-top height and vertical temperature structure detection using GPS radio occultation measurements
Application of data assimilation in the Whole Atmosphere Community Climate Model to the study of day-to-day variability in the middle and upper atmosphere