Abstract
In this study, the performances of variational (three-dimensional variational; 3DVAR), ensemble-based (ensemble Kalman filter; EnKF), and hybrid (E3DVAR) data assimilation (DA) methods based on the Advanced Research Weather Research and Forecasting (WRF) model are investigated over East Asia for two one-month period of January and July in 2016. Before a comparison between three methods for two one-month periods, a single observation experiment is conducted to tune and optimize background error covariance depending on each method, so that all methods have similar influence radius. For a comparison between three methods for two one-month period by assimilating conventional observations, the E3DVAR outperforms 3DVAR and EnKF for both two seasons. The 3DVAR outperforms EnKF in January, whereas EnKF outperforms 3DVAR in July. The root mean of difference total energy (RM-DTE) for January increases as a forecast time increases, saturating at the value less than 5 m s−1. On the contrary, RM-DTE in July keeps increasing until 72 h forecast time reaching at the value less than 7 m s−1. Relatively larger moisture error in initial condition for summer season can grow rapidly and change large-scale feature considerably, which can contribute to the continuous growth of RM-DTE in July. Furthermore, rank histogram and spread statistics results confirm that ensemble spreads are represented reasonably for January and July in 2016, although spreads in July are slightly overestimated compared to those in January. In conclusion, the hybrid DA method (E3DVAR) is the most appropriate among three DA methods over East Asia. In addition, for the better performance, it is necessary to tune and optimize the DA system depending on DA method for the given area.
Original language | English |
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Article number | 105257 |
Journal | Atmospheric Research |
Volume | 249 |
DOIs | |
Publication status | Published - 2021 Feb |
Bibliographical note
Funding Information:The authors appreciate reviewers for their valuable comments. This study was supported by a National Research Foundation of Korea (NRF) grant funded by the South Korean government (Ministry of Science and ICT) (Grant 2017R1E1A1A03070968 ) and the Korea Meteorological Administration Research and Development Program (Grant KMI2018-03712 ). This study was carried out by utilizing the supercomputer system supported by the National Center for Meteorological Supercomputer of Korea Meteorological Administration and Korea Research Environment Open NETwork (KREONET) provided by the Korea Institute of Science and Technology Information. The authors gratefully acknowledge the late Dr. Fuqing Zhang for providing the resources at the earlier stages of this study.
Funding Information:
The authors appreciate reviewers for their valuable comments. This study was supported by a National Research Foundation of Korea (NRF) grant funded by the South Korean government (Ministry of Science and ICT) (Grant 2017R1E1A1A03070968) and the Korea Meteorological Administration Research and Development Program (Grant KMI2018-03712). This study was carried out by utilizing the supercomputer system supported by the National Center for Meteorological Supercomputer of Korea Meteorological Administration and Korea Research Environment Open NETwork (KREONET) provided by the Korea Institute of Science and Technology Information. The authors gratefully acknowledge the late Dr. Fuqing Zhang for providing the resources at the earlier stages of this study.
Publisher Copyright:
© 2020 Elsevier B.V.
All Science Journal Classification (ASJC) codes
- Atmospheric Science