Department of Earth System Science, Ministry of Education Key Laboratory for Earth System Modeling, Institute for Global Change Studies, Tsinghua University, Beijing, 100084, China
Department of Earth System Science, Ministry of Education Key Laboratory for Earth System Modeling, Institute for Global Change Studies, Tsinghua University, Beijing, 100084, China
Li Liu
Department of Earth System Science, Ministry of Education Key Laboratory for Earth System Modeling, Institute for Global Change Studies, Tsinghua University, Beijing, 100084, China
Zheng Fan
Department of Earth System Science, Ministry of Education Key Laboratory for Earth System Modeling, Institute for Global Change Studies, Tsinghua University, Beijing, 100084, China
Department of Earth System Science, Ministry of Education Key Laboratory for Earth System Modeling, Institute for Global Change Studies, Tsinghua University, Beijing, 100084, China
Hong Li
Department of Earth System Science, Ministry of Education Key Laboratory for Earth System Modeling, Institute for Global Change Studies, Tsinghua University, Beijing, 100084, China
Department of Atmospheric and Oceanic Sciences, Institute of
Atmospheric Sciences, Fudan University, Shanghai, 200433, China
Xiang Li
Key Laboratory of Marine Hazards Forecasting, National Marine
Environmental Forecasting Center, Ministry of Natural Resources, Beijing,
100081, China
Yunfei Zhang
Key Laboratory of Marine Hazards Forecasting, National Marine
Environmental Forecasting Center, Ministry of Natural Resources, Beijing,
100081, China
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Total article views: 1,065 (including HTML, PDF, and XML)
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To better understand the effects of surface waves on global intraseasonal prediction, we incorporated the WW3 model into CFSv2.0. Processes of Langmuir mixing, Stokes–Coriolis force with entrainment, air–sea fluxes modified by Stokes drift, and momentum roughness length were considered. Results from two groups of 56 d experiments show that overestimated sea surface temperature, 2 m air temperature, 10 m wind, wave height, and underestimated mixed layer from the original CFSv2.0 are improved.
To better understand the effects of surface waves on global intraseasonal prediction, we...
