Abstract
Assimilation of surface observations including 2-m temperature (T2m) in numerical weather prediction (NWP) models remains a challenging problem owing to differences between the elevation of model terrain and that of actual observation stations. NWP results can be improved only if surface observations are assimilated appropriately. In this study, a T2m data assimilation scheme that carefully considers misrepresentation of model and station terrain was established by using the three-dimensional variational data assimilation (3DVAR) system of the China Meteorological Administration mesoscale model (CMA-MESO). The corresponding forward observation operator, tangent linear operator, and adjoint operator for the T2m observations under three terrain mismatch treatments were developed. The T2m data were assimilated in the same method as that adopted for temperature sounding data with additional representative errors, when station terrain was 100 m higher than model terrain; otherwise, the T2m data were assimilated by using the surface similarity theory assimilation operator. Furthermore, if station terrain was lower than model terrain, additional representative errors were stipulated and corrected. Test of a rainfall case showed that the observation innovation and analysis residuals both exhibited Gaussian distribution and that the analysis increment was reasonable. Moreover, it was found that on completion of the data assimilation cycle, T2m data assimilation obviously influenced the temperature, wind, and relative humidity fields throughout the troposphere, with the greatest impact evident in the lower layers, and that both the area and the intensity of rainfall were better forecasted, especially for the first 12 hours. Long-term continuous experiments for 2–28 February and 5–20 July 2020, further verified that T2m data assimilation reduced deviations not only in T2m but also in 10-m wind forecasts. More importantly, the precipitation equitable threat scores were improved over the two experimental periods. In summary, this study confirmed that the T2m data assimilation scheme that we implemented in the kilometer-scale CMA-MESO 3DVAR system is effective.
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Acknowledgments
We are grateful to Dr. Yongzhu Liu from the China Meteorological Administration’s Earth System Numerical Prediction Centre who contributed to the completion of this work. We thank the anonymous reviewers and editors for their thoughtful comments that helped us to improve the manuscript.
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Supported by the National Key Research and Development Program of China (2018YFF0300103).
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Xu, Z., Zhang, L., Wang, R. et al. Effect of 2-m Temperature Data Assimilation in the CMA-MESO 3DVAR System. J Meteorol Res 37, 218–233 (2023). https://doi.org/10.1007/s13351-023-2115-9
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DOI: https://doi.org/10.1007/s13351-023-2115-9