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Titlebook: New Horizons in Occultation Research; Studies in Atmospher Andrea Steiner,Barbara Pirscher,Gottfried Kircheng Book 20091st edition Springer

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GPS Radio Occultation with CHAMP, GRACE-A, SAC-C, TerraSAR-X, and FORMOSAT-3/COSMIC: Brief Review ofserving System for Meteorology, Ionosphere, and Climate), and MetOp) started data provision in 2006 and 2007. Together with the measurements from CHAMP (CHAllenging Minisatellite Payload, since 2001) and the recently launched (June 15, 2007) TerraSAR-X an operational multi-satellite constellation fo
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Error Estimate of Bending Angles in the Presence of Strong Horizontal Gradientsng angle from radio occultation data. This technique can be universally applied for the (hypothetical) spherically-symmetric atmosphere and any multipath situation can be unfolded. The reason is that the CT/FSI technique uses a Fourier Integral Operator that maps the measured wave field into the imp
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Using Airborne GNSS Receivers to Detect Atmospheric Turbulencecattering theory for electromagnetic wave propagation in random media. These techniques are modified to deal with a transmitter and receiver moving relative to each other. A simulation method is then used to evaluate the sensitivity of the intensity estimates to two other unknown parameters, the tur
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The GRAS SAF Radio Occultation Processing Intercomparison Project ROPICed for numerical weather prediction, atmospheric process studies, and climate research. Especially in the latter case it is important to fully understand the influence of the particular processing (algorithms, implementations, and used parameters) on the quantities used for further studies. To asses
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Radio Occultation Soundings in Ionosphere and Space Weather Applications: Achievements and Prospectst on their way from the transmitter to the receiver. The impact of the ionosphere is an error source that is usually eliminated in the ground based GNSS navigation applications and in the retrieval of the characteristics of the neutral atmosphere from the RO (Radio Occultation) soundings. However, b
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Retrieval of Trace Gas Concentrations from Lunar Occultation Measurements with SCIAMACHY on ENVISATatmospheric trace gas distributions in nadir, limb, and occultation geometries. In occultation mode, SCIAMACHY tracks the rising Sun or Moon directly through the atmosphere. Dividing the atmospheric measurements by extraterrestrial references gives transmission spectra, which are suitable for a DOAS
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