IIOn the extension of the freak wave warning system and its verificationLow‐level jets over the North Sea based on ERA5 and observations: together they do betterPossible artifacts of data biases in the recent global surface warming hiatusEffects of all‐sky assimilation of GCOM‐W/AMSR2 radiances in the ECMWF numerical weather prediction systemToward a consistent reanalysis of the upper stratosphere based on radiance measurements from SSU and AMSU‐AThe JRA‐55 reanalysis: general specifications and basic characteristicsAssimilation of Geostationary WV Radiances from GOES and Meteosat at ECMWFCERA‐20C: a coupled reanalysis of the twentieth centuryEvaluation and assimilation of the Microwave Sounder MWHS‐2 onboard FY‐3C in the ECMWF numerical weather prediction systemSorce contributions to new understanding of global change and solar variabilityMonitoring and operational assimilation of Himawari‐9 clear‐sky geostationary radiancesStochastic representations of model uncertainties at ECMWF: state of the art and future visionClimatology and interannual variability of dynamic variables in multiple reanalyses evaluated by the SPARC Reanalysis Intercomparison Project (S‐RIP)Direct 4D‐Var assimilation of NCEP Stage IV radar and gauge precipitation data at ECMWFAssimilation of cloud‐affected radiances from Meteosat‐9 at ECMWFAn alternative cell‐averaged departure point reconstruction for pointwise semi‐Lagrangian transport schemesRepresenting land surface heterogeneity: offline analysis of the tiling methodRevisiting the mystery of recent stratospheric temperature trendsPoleward atmospheric energy transports and their variability as evaluated from ECMWF reanalysis dataAn improved estimate of the coupled Arctic energy budgetA cloud detection algorithm for high‐spectral‐resolution infrared soundersThe version 8.6 SBUV ozone data record: an overviewSea surface temperature datasets for climate applications from Phase 1 of the European Space Agency Climate Change Initiative (SST CCI)Implementation of the lake parameterisation scheme FLake into the numerical weather prediction model COSMORadiation and cloud radiative properties in the European Centre for Medium Range Weather Forecasts forecasting systemImpact of a new radiation package, McRad, in the ECMWF Integrated Forecasting SystemQuantifying uncertainties in global and regional temperature change using an ensemble of observational estimates: the HadCRUT4 data setCharacterization of the impact of geostationary clear‐sky radiances on wind analyses in a 4D‐Var contextA review of Stratospheric Sounding Unit radiance observations for climate trends and reanalysesImproved middle atmosphere climate and forecasts in the ECMWF model through a non‐orographic gravity wave drag parameterizationCoupled data assimilation for Integrated Earth System Analysis and Prediction: Goals, challenges, and recommendationsCharacterization of the impact of geostationary clear‐sky radiances on wind analyses in a 4D‐Var contextA fast, flexible, approximate technique for computing radiative transfer in inhomogeneous cloudsERA‐20C: an atmospheric reanalysis of the twentieth centuryQuality control, error analysis, and impact assessment of FORMOSAT‐3/COSMIC in numerical weather predictionStratospheric temperature trends over 1979–2015 derived from combined SSU, MLS, and SABER satellite observationsAtmospheric Motion Vector observations in the ECMWF system: Fifth year report 41Why is it so difficult to represent stably stratified conditions in numerical weather prediction (NWP) models?An update on the RTTOV fast radiative transfer model (currently at version 12)Temperature trends derived from Stratospheric Sounding Unit radiances: The effect of increasing COECMWF analyses and forecasts of stratospheric winter polar vortex breakup: September 2002 in the Southern Hemisphere and related eventsLow‐frequency variations in surface atmospheric humidity, temperature and precipitation: inferences from reanalyses and monthly gridded observational datasetsEstimating low‐frequency variability and trends in atmospheric temperature from the ERA‐Interim reanalysisA reassessment of temperature variations and trends from global reanalyses and monthly surface climatological datasetsGlobal stratospheric temperature bias and other stratospheric aspects of ERA5 and ERA5.1Scatterometer data interpretation: estimation and validation of the transfer function CMOD4Maintaining atmospheric mass and water balance in reanalysesEvaluation of the ERA5 reanalysis as a potential reference dataset for hydrological modeling over North AmericaOn the use of a Huber norm for observation quality control in the ECMWF 4D‐VarA validation of ERA5 reanalysis data in the Southern Antarctic peninsula – Ellsworth Land region, and its implications for ice core studiesThe Copernicus programme and its climate change service.
In ERA‐Interim, soil moisture and soil temperature simulations are corrected by the 2‐m analysis increments of air temperature and relative humidity, according to an empirical approach.
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