A First Evaluation of ERA-20CM over China
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Allen, 2010, Explosive cyclogenesis: A global climatology comparing multiple reanalyses, J. Climate, 23, 6468, 10.1175/2010JCLI3437.1
Bao, 2013, Evaluation of NCEP–CFSR, NCEP–NCAR, ERA-Interim, and ERA-40 reanalysis datasets against independent sounding observations over the Tibetan Plateau, J. Climate, 26, 206, 10.1175/JCLI-D-12-00056.1
Berg, 2003, Impact of bias correction to reanalysis products on simulations of North American soil moisture and hydrological fluxes, J. Geophys. Res., 108, 4490, 10.1029/2002JD003334
Betts, 2009, Comparison of river basin hydrometeorology in ERA-Interim and ERA-40 reanalyses with observations, J. Geophys. Res., 114, D02101, 10.1029/2008JD010761
Bosilovich, 2008, Evaluation of global precipitation in reanalyses, J. Appl. Meteor. Climatol., 47, 2279, 10.1175/2008JAMC1921.1
Cardinali, 2014, Impact of GPS radio occultation measurements in the ECMWF system using adjoint-based diagnostics, Quart. J. Roy. Meteor. Soc., 140, 2315, 10.1002/qj.2300
Decker, 2012, Evaluation of the reanalysis products from GSFC, NCEP, and ECMWF using flux tower observations, J. Climate, 25, 1916, 10.1175/JCLI-D-11-00004.1
Frauenfeld, 2005, Climate change and variability using European Centre for Medium-Range Weather Forecasts reanalysis (ERA-40) temperatures on the Tibetan Plateau, J. Geophys. Res., 110, D02101, 10.1029/2004JD005230
Gao, L. , 2013: Validation and statistical downscaling of ERA-Interim reanalysis data for integrated applications. Ph.D. dissertation, Ludwig-Maximilians-Universität München, 193 pp. [Available online at http://edoc.ub.uni-muenchen.de/17317/.]
Gao, 2012, Elevation correction of ERA-Interim temperature data in complex terrain, Hydrol. Earth Syst. Sci., 16, 4661, 10.5194/hess-16-4661-2012
Gao, 2014, Statistical downscaling of ERA-Interim forecast precipitation data in complex terrain using LASSO algorithm, Adv. Meteor., 2014, 472741, 10.1155/2014/472741
Gao, 2014, Evaluation of ERA-Interim monthly temperature data over the Tibetan Plateau, J. Mt. Sci., 11, 1154, 10.1007/s11629-014-3013-5
Hersbach, 2013
Hersbach, 2015, ERA-20CM: A twentieth-century atmospheric model ensemble, Quart. J. Roy. Meteor. Soc., 141, 2350, 10.1002/qj.2528
Hodges, 2011, A comparison of extratropical cyclones in recent reanalyses ERA-Interim, NASA MERRA, NCEP CFSR, and JRA-25, J. Climate, 24, 4888, 10.1175/2011JCLI4097.1
Mao, 2010, Assessment of reanalysis daily extreme temperatures with China’s homogenized historical dataset during 1979–2001 using probability density functions, J. Climate, 23, 6605, 10.1175/2010JCLI3581.1
Pappenberger, 2015, How do I know if my forecasts are better? Using benchmarks in Hydrological Ensemble Prediction, J. Hydrol., 522, 697, 10.1016/j.jhydrol.2015.01.024
Perkins, 2007, Evaluation of the AR4 climate models’ simulated daily maximum temperature, minimum temperature, and precipitation over Australia using probability density functions, J. Climate, 20, 4356, 10.1175/JCLI4253.1
Shi, 2007, Regional characteristics of the interdecadal turning of winter/summer climate modes in Chinese mainland, Chin. Sci. Bull., 52, 101, 10.1007/s11434-007-0007-5
Simmons, 2004, Comparison of trends and low-frequency variability in CRU, ERA-40, and NCEP/NCAR analyses of surface air temperature, J. Geophys. Res., 109, D24115, 10.1029/2004JD005306
Simmons, 2010, Low-frequency variations in surface atmospheric humidity, temperature, and precipitation: Inferences from reanalyses and monthly gridded observational data sets, J. Geophys. Res., 115, D01110, 10.1029/2009JD012442
Titchner, 2014, The Met Office Hadley Centre sea ice and sea surface temperature data set, version 2: 1. Sea ice concentrations, J. Geophys. Res. Atmos., 119, 2864, 10.1002/2013JD020316
Trenberth, 1998, Evaluation of the atmospheric moisture and hydrological cycle in the NCEP/NCAR reanalyses, Climate Dyn., 14, 213, 10.1007/s003820050219
Trenberth, 2008, Progress and prospects for reanalysis for weather and climate, Eos, Trans. Amer. Geophys. Union, 89, 234, 10.1029/2008EO260002