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Papers by Guifu Zhang

Research paper thumbnail of On the Influence of Assumed Drop Size Distribution Form on Radar-Retrieved Thunderstorm Microphysics

Journal of Applied Meteorology and Climatology, Feb 1, 2006

Research paper thumbnail of On the Influence of Assumed Drop Size Distribution Form on Radar-Retrieved Thunderstorm Microphysics

Journal of Applied Meteorology and Climatology, Feb 1, 2006

Research paper thumbnail of Comments on “Describing the Shape of Raindrop Size Distributions Using Uncorrelated Raindrop Mass Spectrum Parameters”

Journal of Applied Meteorology and Climatology, 2015

Research paper thumbnail of Reducing the effects of noise on atmospheric imaging radars using multilag correlation

Research paper thumbnail of Diagnosing the intercept parameters of the exponential drop size distributions in a single-moment microphysics scheme and impact on supercell storm simulations

Journal of Applied Meteorology and Climatology, 2014

Research paper thumbnail of The Analysis and Prediction of Microphysical States and Polarimetric Radar Variables in a Mesoscale Convective System Using Double-Moment Microphysics, Multinetwork Radar Data, and the Ensemble Kalman Filter

Monthly Weather Review, 2014

Doppler radar data are assimilated with an ensemble Kalman Filter (EnKF) in combination with a do... more Doppler radar data are assimilated with an ensemble Kalman Filter (EnKF) in combination with a double-moment (DM) microphysics scheme in order to improve the analysis and forecast of microphysical states and precipitation structures within a mesoscale convective system (MCS) that passed over western Oklahoma on 8–9 May 2007. Reflectivity and radial velocity data from five operational Weather Surveillance Radar-1988 Doppler (WSR-88D) S-band radars as well as four experimental Collaborative and Adaptive Sensing of the Atmosphere (CASA) X-band radars are assimilated over a 1-h period using either single-moment (SM) or DM microphysics schemes within the forecast ensemble. Three-hour deterministic forecasts are initialized from the final ensemble mean analyses using a SM or DM scheme, respectively. Polarimetric radar variables are simulated from the analyses and compared with polarimetric WSR-88D observations for verification. EnKF assimilation of radar data using a multimoment microphys...

Research paper thumbnail of Incorporating NASA Spaceborne Radar Data into NOAA National Mosaic QPE System for Improved Precipitation Measurement: A Physically Based VPR Identification and Enhancement Method

Journal of Hydrometeorology, 2013

This study proposes an approach that identifies and corrects for the vertical profile of reflecti... more This study proposes an approach that identifies and corrects for the vertical profile of reflectivity (VPR) by using Tropical Rainfall Measuring Mission (TRMM) precipitation radar (PR) measurements in the region of Arizona and southern California, where the ground-based Next Generation Weather Radar (NEXRAD) finds difficulties in making reliable estimations of surface precipitation amounts because of complex terrain and limited radar coverage. A VPR identification and enhancement (VPR-IE) method based on the modeling of the vertical variations of the equivalent reflectivity factor using a physically based parameterization is employed to obtain a representative VPR at S band from the TRMM PR measurement at Ku band. Then the representative VPR is convolved with ground radar beam sampling properties to compute apparent VPRs for enhancing NEXRAD quantitative precipitation estimation (QPE). The VPR-IE methodology is evaluated with several stratiform precipitation events during the cold s...

Research paper thumbnail of On the Influence of Assumed Drop Size Distribution Form on Radar-Retrieved Thunderstorm Microphysics

Journal of Applied Meteorology and Climatology, 2006

Polarimetric radar measurements are used to retrieve drop size distributions (DSD) in subtropical... more Polarimetric radar measurements are used to retrieve drop size distributions (DSD) in subtropical thunderstorms. Retrievals are made with the single-moment exponential drop size model of Marshall and Palmer driven by radar reflectivity measurements and with a two-parameter constrained-gamma drop size model that utilizes reflectivity and differential reflectivity. Results are compared with disdrometer observations. Retrievals with the constrained-gamma DSD model gave better representation of total drop concentration, liquid water content, and drop median volume diameter and better described their natural variability. The Marshall–Palmer DSD model, with a fixed intercept parameter, tended to underestimate the total drop concentration in storm cores and to overestimate significantly the concentration in stratiform regions. Rainwater contents in strong convection were underestimated by a factor of 2–3, and drop median volume diameters in stratiform rain were underestimated by 0.5 mm. To...

Research paper thumbnail of Drop Size Distribution Retrieval with Polarimetric Radar: Model and Application

Journal of Applied Meteorology, 2004

Research paper thumbnail of A method for estimating rain rate and drop size distribution from polarimetric radar measurements

IEEE Transactions on Geoscience and Remote Sensing, 2001

Research paper thumbnail of Retrieval of atmospheric liquid and ice characteristics using dual-wavelength radar observations

IEEE Transactions on Geoscience and Remote Sensing, 1999

Research paper thumbnail of Experiments in rainfall estimation with a polarimetric radar in a subtropical environment

Journal of Applied …, 2002

Research paper thumbnail of Radar reflectivity calibration using differential propagation phase measurement

Research paper thumbnail of A statistical and physical description of hydrometeor distributions in Colorado snowstorms using a video disdrometer

Research paper thumbnail of Improving parameterization of rain microphysics with disdrometer and radar observations

Research paper thumbnail of Ensemble Kalman Filter Analyses of the 29―30 May 2004 Oklahoma Tornadic Thunderstorm Using One-and Two-Moment Bulk Microphysics Schemes, with Verification against Polarimetric Radar Data

Research paper thumbnail of Simulations of polarimetric radar signatures of a supercell storm using a two-moment bulk microphysics scheme

Research paper thumbnail of Error modeling of simulated reflectivity observations for ensemble Kalman filter assimilation of convective storms

Research paper thumbnail of Assimilation of simulated polarimetric radar data for a convective storm using the ensemble Kalman filter. Part I: Observation operators for reflectivity and polarimetric variables

Research paper thumbnail of Simultaneous estimation of microphysical parameters and atmospheric state with simulated radar data and ensemble square root Kalman filter. Part I: Sensitivity analysis and parameter identifiability

Research paper thumbnail of On the Influence of Assumed Drop Size Distribution Form on Radar-Retrieved Thunderstorm Microphysics

Journal of Applied Meteorology and Climatology, Feb 1, 2006

Research paper thumbnail of On the Influence of Assumed Drop Size Distribution Form on Radar-Retrieved Thunderstorm Microphysics

Journal of Applied Meteorology and Climatology, Feb 1, 2006

Research paper thumbnail of Comments on “Describing the Shape of Raindrop Size Distributions Using Uncorrelated Raindrop Mass Spectrum Parameters”

Journal of Applied Meteorology and Climatology, 2015

Research paper thumbnail of Reducing the effects of noise on atmospheric imaging radars using multilag correlation

Research paper thumbnail of Diagnosing the intercept parameters of the exponential drop size distributions in a single-moment microphysics scheme and impact on supercell storm simulations

Journal of Applied Meteorology and Climatology, 2014

Research paper thumbnail of The Analysis and Prediction of Microphysical States and Polarimetric Radar Variables in a Mesoscale Convective System Using Double-Moment Microphysics, Multinetwork Radar Data, and the Ensemble Kalman Filter

Monthly Weather Review, 2014

Doppler radar data are assimilated with an ensemble Kalman Filter (EnKF) in combination with a do... more Doppler radar data are assimilated with an ensemble Kalman Filter (EnKF) in combination with a double-moment (DM) microphysics scheme in order to improve the analysis and forecast of microphysical states and precipitation structures within a mesoscale convective system (MCS) that passed over western Oklahoma on 8–9 May 2007. Reflectivity and radial velocity data from five operational Weather Surveillance Radar-1988 Doppler (WSR-88D) S-band radars as well as four experimental Collaborative and Adaptive Sensing of the Atmosphere (CASA) X-band radars are assimilated over a 1-h period using either single-moment (SM) or DM microphysics schemes within the forecast ensemble. Three-hour deterministic forecasts are initialized from the final ensemble mean analyses using a SM or DM scheme, respectively. Polarimetric radar variables are simulated from the analyses and compared with polarimetric WSR-88D observations for verification. EnKF assimilation of radar data using a multimoment microphys...

Research paper thumbnail of Incorporating NASA Spaceborne Radar Data into NOAA National Mosaic QPE System for Improved Precipitation Measurement: A Physically Based VPR Identification and Enhancement Method

Journal of Hydrometeorology, 2013

This study proposes an approach that identifies and corrects for the vertical profile of reflecti... more This study proposes an approach that identifies and corrects for the vertical profile of reflectivity (VPR) by using Tropical Rainfall Measuring Mission (TRMM) precipitation radar (PR) measurements in the region of Arizona and southern California, where the ground-based Next Generation Weather Radar (NEXRAD) finds difficulties in making reliable estimations of surface precipitation amounts because of complex terrain and limited radar coverage. A VPR identification and enhancement (VPR-IE) method based on the modeling of the vertical variations of the equivalent reflectivity factor using a physically based parameterization is employed to obtain a representative VPR at S band from the TRMM PR measurement at Ku band. Then the representative VPR is convolved with ground radar beam sampling properties to compute apparent VPRs for enhancing NEXRAD quantitative precipitation estimation (QPE). The VPR-IE methodology is evaluated with several stratiform precipitation events during the cold s...

Research paper thumbnail of On the Influence of Assumed Drop Size Distribution Form on Radar-Retrieved Thunderstorm Microphysics

Journal of Applied Meteorology and Climatology, 2006

Polarimetric radar measurements are used to retrieve drop size distributions (DSD) in subtropical... more Polarimetric radar measurements are used to retrieve drop size distributions (DSD) in subtropical thunderstorms. Retrievals are made with the single-moment exponential drop size model of Marshall and Palmer driven by radar reflectivity measurements and with a two-parameter constrained-gamma drop size model that utilizes reflectivity and differential reflectivity. Results are compared with disdrometer observations. Retrievals with the constrained-gamma DSD model gave better representation of total drop concentration, liquid water content, and drop median volume diameter and better described their natural variability. The Marshall–Palmer DSD model, with a fixed intercept parameter, tended to underestimate the total drop concentration in storm cores and to overestimate significantly the concentration in stratiform regions. Rainwater contents in strong convection were underestimated by a factor of 2–3, and drop median volume diameters in stratiform rain were underestimated by 0.5 mm. To...

Research paper thumbnail of Drop Size Distribution Retrieval with Polarimetric Radar: Model and Application

Journal of Applied Meteorology, 2004

Research paper thumbnail of A method for estimating rain rate and drop size distribution from polarimetric radar measurements

IEEE Transactions on Geoscience and Remote Sensing, 2001

Research paper thumbnail of Retrieval of atmospheric liquid and ice characteristics using dual-wavelength radar observations

IEEE Transactions on Geoscience and Remote Sensing, 1999

Research paper thumbnail of Experiments in rainfall estimation with a polarimetric radar in a subtropical environment

Journal of Applied …, 2002

Research paper thumbnail of Radar reflectivity calibration using differential propagation phase measurement

Research paper thumbnail of A statistical and physical description of hydrometeor distributions in Colorado snowstorms using a video disdrometer

Research paper thumbnail of Improving parameterization of rain microphysics with disdrometer and radar observations

Research paper thumbnail of Ensemble Kalman Filter Analyses of the 29―30 May 2004 Oklahoma Tornadic Thunderstorm Using One-and Two-Moment Bulk Microphysics Schemes, with Verification against Polarimetric Radar Data

Research paper thumbnail of Simulations of polarimetric radar signatures of a supercell storm using a two-moment bulk microphysics scheme

Research paper thumbnail of Error modeling of simulated reflectivity observations for ensemble Kalman filter assimilation of convective storms

Research paper thumbnail of Assimilation of simulated polarimetric radar data for a convective storm using the ensemble Kalman filter. Part I: Observation operators for reflectivity and polarimetric variables

Research paper thumbnail of Simultaneous estimation of microphysical parameters and atmospheric state with simulated radar data and ensemble square root Kalman filter. Part I: Sensitivity analysis and parameter identifiability

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