Assimilation of Global Positioning System radio occultation data in the ECMWF ERA–Interim reanalysis

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GPS radio occultation for climate monitoring and change detection (2011, background): “ERA‐Interim shows a characteristic warming/cooling feature above/below 150 hPa, which is a peculiarity of this reanalysis [Poli et al., 2010].”
Introduction to the SPARC Reanalysis Intercomparison Project (S-RIP) and overview of the reanalysis systems (2016, background): “ERA-20Ca Poli et al. (2016) Centre: ECMWF Coverage: January 1900 to December 2010”
Homogenization of the Global Radiosonde Temperature Dataset through Combined Comparison with Reanalysis Background Series and Neighboring Stations (2012, methodology): “Warming relative toRAOBCOREoccurs in 2007, when data from the Constellation Observing System for Meteorology, Ionosphere and Climate (COSMIC) have been introduced in ERA-Interim (Poli et al. 2010).”
A review of the remote sensing of lower tropospheric thermodynamic profiles and its indispensable role for the understanding and the simulation of water and energy cycles (2015, methodology): “Particularly, RO data have been successfully applied to global DA [Cucurull et al., 2007; Healy et al., 2007; Poli et al., 2010].”