TY - JOUR
T1 - Assimilating GNSS PWV and radiosonde meteorological profiles to improve the PWV and rainfall forecasting performance from the Weather Research and Forecasting (WRF) model over the South China
AU - Gong, Yangzhao
AU - Liu, Zhizhao
AU - Chan, Pak Wai
AU - Hon, Kai Kwong
N1 - Funding Information:
This work was supported by the Hong Kong Research Grants Council (RGC) (Q73B, PolyU 15211919 and Q80Q, PolyU 15221620) and the Emerging Frontier Area (EFA) Scheme of Research Institute for Sustainable Urban Development (RISUD) of the Hong Kong Polytechnic University (No. 1-BBWJ). The National Centers for Environmental Prediction (NCEP) is appreciated for providing the Global Forecast System (GFS) data. GFS data can be downloaded from the Research Data Archive (RDA) managed by Data Engineering and Curation Section (DECS) of the Computational and Information Systems Laboratory (CISL) (https://rda.ucar.edu/datasets/ds084.1/). The authors thank GNSS data product service platform of China Earthquake Administration for providing GNSS water vapor data of the Crustal Movement Observation Network Of China (CMONOC). We thank the China Meteorological Administration for providing the China Meteorological Administration GNSS Network (CMAGN) water vapor products. GNSS water vapor data used in this study are available on request from the authors. The National Oceanic and Atmospheric Administration (NOAA) is thanked for providing the Integrated Global Radiosonde Archive (IGRA) radiosonde data. IGRA radiosonde data can be downloaded via ftp://ftp.ncdc.noaa.gov/pub/data/igra/. We thank the China Meteorological Data Service Center for providing rainfall data (https://data.cma.cn/).
Funding Information:
This work was supported by the Hong Kong Research Grants Council (RGC) ( Q73B, PolyU 15211919 and Q80Q, PolyU 15221620 ) and the Emerging Frontier Area (EFA) Scheme of Research Institute for Sustainable Urban Development (RISUD) of the Hong Kong Polytechnic University (No. 1-BBWJ ). The National Centers for Environmental Prediction (NCEP) is appreciated for providing the Global Forecast System (GFS) data. GFS data can be downloaded from the Research Data Archive (RDA) managed by Data Engineering and Curation Section (DECS) of the Computational and Information Systems Laboratory (CISL) ( https://rda.ucar.edu/datasets/ds084.1/ ). The authors thank GNSS data product service platform of China Earthquake Administration for providing GNSS water vapor data of the Crustal Movement Observation Network Of China (CMONOC). We thank the China Meteorological Administration for providing the China Meteorological Administration GNSS Network (CMAGN) water vapor products. GNSS water vapor data used in this study are available on request from the authors. The National Oceanic and Atmospheric Administration (NOAA) is thanked for providing the Integrated Global Radiosonde Archive (IGRA) radiosonde data. IGRA radiosonde data can be downloaded via ftp://ftp.ncdc.noaa.gov/pub/data/igra/ . We thank the China Meteorological Data Service Center for providing rainfall data ( https://data.cma.cn/ ).
Publisher Copyright:
© 2023 Elsevier B.V.
PY - 2023/5/1
Y1 - 2023/5/1
N2 - Precipitable Water Vapor (PWV) and rainfall play important roles in the meteorological processes. In this study, we have investigated the impact of assimilation of Global Navigation Satellite System (GNSS) PWV and radiosonde profiles on the performance of Weather Research and Forecasting (WRF) model in forecasting PWV and rainfall over the South China region for April 01, 2020 to May 31, 2020. PWV observations derived from 213 GNSS stations and meteorological profiles recorded by 23 radiosonde stations are assimilated into WRF model. Five different WRF schemes are adopted: WRF scheme 0: no data assimilation (DA); WRF scheme 1: assimilation of PWV from 76 GNSS stations; WRF scheme 2: assimilation of PWV from 213 GNSS stations; WRF scheme 3: assimilation of meteorological profiles from 23 radiosonde stations; WRF scheme 4: assimilation of both PWV from 213 GNSS stations and meteorological profiles from 23 radiosonde stations. PWV observations derived from 170 independent GNSS (have not been used in assimilation) and rainfall data recorded by 648 surface meteorological stations are used to evaluate WRF forecasting performance in PWV and rainfall, respectively. The results indicate that all DA schemes improve the WRF forecasting performance for both PWV and rainfall. For the first 6 h after data assimilation, WRF schemes 1 to 4 improve the PWV forecasting accuracy by 11.6%, 14.5%, 2.9%, and 14.8%, respectively. For the accumulated rainfall within the first 6 h after data assimilation, WRF scheme 2 and WRF scheme 4 have a similar performance and outperform other DA schemes while the WRF scheme 4 is the best one among all five schemes. WRF scheme 4 improves the rainfall forecast probability of detection and equitable threat score by 0.085 and 0.057, respectively.
AB - Precipitable Water Vapor (PWV) and rainfall play important roles in the meteorological processes. In this study, we have investigated the impact of assimilation of Global Navigation Satellite System (GNSS) PWV and radiosonde profiles on the performance of Weather Research and Forecasting (WRF) model in forecasting PWV and rainfall over the South China region for April 01, 2020 to May 31, 2020. PWV observations derived from 213 GNSS stations and meteorological profiles recorded by 23 radiosonde stations are assimilated into WRF model. Five different WRF schemes are adopted: WRF scheme 0: no data assimilation (DA); WRF scheme 1: assimilation of PWV from 76 GNSS stations; WRF scheme 2: assimilation of PWV from 213 GNSS stations; WRF scheme 3: assimilation of meteorological profiles from 23 radiosonde stations; WRF scheme 4: assimilation of both PWV from 213 GNSS stations and meteorological profiles from 23 radiosonde stations. PWV observations derived from 170 independent GNSS (have not been used in assimilation) and rainfall data recorded by 648 surface meteorological stations are used to evaluate WRF forecasting performance in PWV and rainfall, respectively. The results indicate that all DA schemes improve the WRF forecasting performance for both PWV and rainfall. For the first 6 h after data assimilation, WRF schemes 1 to 4 improve the PWV forecasting accuracy by 11.6%, 14.5%, 2.9%, and 14.8%, respectively. For the accumulated rainfall within the first 6 h after data assimilation, WRF scheme 2 and WRF scheme 4 have a similar performance and outperform other DA schemes while the WRF scheme 4 is the best one among all five schemes. WRF scheme 4 improves the rainfall forecast probability of detection and equitable threat score by 0.085 and 0.057, respectively.
KW - Data assimilation
KW - Global Navigation Satellite System (GNSS)
KW - Precipitable water vapor
KW - Radiosonde
KW - Weather Research and Forecasting (WRF) Model
UR - http://www.scopus.com/inward/record.url?scp=85148543820&partnerID=8YFLogxK
U2 - 10.1016/j.atmosres.2023.106677
DO - 10.1016/j.atmosres.2023.106677
M3 - Journal article
AN - SCOPUS:85148543820
SN - 0169-8095
VL - 286
JO - Atmospheric Research
JF - Atmospheric Research
M1 - 106677
ER -