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In addition, our analysis shows that RO data above 30 km height becomes dubious for gravity waves potential energy calculations.
'Onion-peeling' is a very common technique used to invert Radio Occultation (RO) data in the ionosphere.
RO data from 30 consecutive days during July and August 2006 are divided into ten groups in terms of daytime or nighttime and latitude.
In this study we apply the new method to the RO data sets from CHAMP/GRACE (2001 2009) and FORMOSAT-3/COSMIC (2006–2009).
The results are encouraging for future large-scale use of RO data for supporting the monitoring of volcanic clouds and their impacts on weather and climate.
The FORMOSAT-3/COSMIC mission which is a joint Taiwan-US mission for meteorological, climatological, ionospheric, and geodetic studies has successfully provided a significant amount of GPS radio occultation (RO) data for better modeling of climate model, forecasting of weather, and monitoring of ionosphere.
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"Data analysis" section outlines the three retrievals of the GPS-RO data, while "Results and discussion" section compares the T profiles in terms of the CPT and LRT among the three GPS-RO datasets.
Arras et al. (2009) also showed semidiurnal tidal signature on the variability of Es occurrences from GPS-RO data.
The fundamental retrieval techniques for the GPS-RO data are geometric optics (GO) and wave optics (WO), assuming that the atmosphere has spherical symmetry (Melbourne 2004).
The long-term GPS-RO data indicate climate change signals from warming in the upper troposphere and cooling in the lower stratosphere (Steiner et al. 2011).
In the next subsection, we compare these GPS-RO data with simultaneous radiosondes to ascertain which products are closer to the real atmosphere.
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