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modeling system (HL-RMS) of the US National Weather Service . J. Hydrol. , 291 , 297 – 318 , doi: 10.1016/j.jhydrol.2003.12.039 . Koren, V. , Smith M. , Cui Z. , and Cosgrove B. , 2007 : Physically-based modifications to the Sacramento Soil Moisture Accounting model: Modeling the effects of frozen ground on the rainfall–runoff process. NOAA Tech. Rep. NWS 52, 43 pp. [Available online at www.nws.noaa.gov/oh/hrl/hsmb/docs/hydrology/PBE_SAC-SMA/NOAA_Technical_Report_NWS_52.pdf .] Kuzmin, V
modeling system (HL-RMS) of the US National Weather Service . J. Hydrol. , 291 , 297 – 318 , doi: 10.1016/j.jhydrol.2003.12.039 . Koren, V. , Smith M. , Cui Z. , and Cosgrove B. , 2007 : Physically-based modifications to the Sacramento Soil Moisture Accounting model: Modeling the effects of frozen ground on the rainfall–runoff process. NOAA Tech. Rep. NWS 52, 43 pp. [Available online at www.nws.noaa.gov/oh/hrl/hsmb/docs/hydrology/PBE_SAC-SMA/NOAA_Technical_Report_NWS_52.pdf .] Kuzmin, V
precipitation, but also an estimate of uncertainty of the retrieval itself (see Elsaesser and Kummerow 2015 ). The GPROF retrieval scheme has undergone a number of modifications over time to improve the retrievals, including improvements to the radiative transfer model used in the generation of the a priori database, freezing-level heights over the oceans, discrimination of regions of stratiform versus convective precipitation, cold surface screening, etc. (see Kummerow et al. 2001 ). The current GPROF
precipitation, but also an estimate of uncertainty of the retrieval itself (see Elsaesser and Kummerow 2015 ). The GPROF retrieval scheme has undergone a number of modifications over time to improve the retrievals, including improvements to the radiative transfer model used in the generation of the a priori database, freezing-level heights over the oceans, discrimination of regions of stratiform versus convective precipitation, cold surface screening, etc. (see Kummerow et al. 2001 ). The current GPROF
