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作 者:Yifan ZHAO Xindong PENG Dehui CHEN Yerong FENG Xiaohan LI Juan GU
机构地区:[1]State Key Laboratory of Severe Weather,Chinese Academy of Meteorological Sciences,China Meteorological Administration,Beijing 100081 [2]College of Earth and Planetary Sciences,University of Chinese Academy of Sciences,Beijing 100190 [3]CMA Earth System Modeling and Prediction Centre,China Meteorological Administration(CMA),Beijing 100081 [4]Guangzhou Institute of Tropical and Marine Meteorology,China Meteorological Administration,Guangzhou 510640 [5]College of Aviation Meteorology,Civil Aviation Flight University of China,Guanghan 618307
出 处:《Journal of Meteorological Research》2024年第5期901-922,共22页气象学报(英文版)
基 金:Supported by the National Natural Science Foundation of China(42375153,42075151,and 42205157).
摘 要:The definition of a reference state close to the realistic atmosphere in an atmospheric model is essential for deriving prognostic deviations and improving numerical accuracy.In this study,a new dynamical framework allowing easy switching between a one-dimensional(1D)and a three-dimensional(3D)time-independent reference state is developed for the semi-implicit semi-Lagrangian solver in a global non-hydrostatic atmospheric model on Yin–Yang grids.The 3D reference state is introduced with consideration of additional horizontal gradient terms of referencestate terms,which is different from the 1D reference state.It is characterized by reduced magnitude of deviations,more accurate pressure gradient force,as well as alleviated numerical noise.Four idealized benchmark tests and multiple full-physics real-case forecasts are carried out to assess the impact of the 3D and 1D reference states.The 3D reference state shows significant advantages in the simulation of atmospheric transport and wave propagation in the idealized experiments.In the real-case forecasts,batched forecasts from June to August 2021 show a comprehensive improvement in medium-range prediction by using the 3D reference state.The new scheme achieves an enhanced prediction skill for large-scale circulation and extends the effective forecast period by 0.8 days in the Northern Hemisphere.
关 键 词:semi-implicit semi-Lagrange three-dimensional reference state global non-hydrostatic atmospheric model linearized equation medium-range weather prediction
分 类 号:P431[天文地球—大气科学及气象学] P456
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