Currently I am working on a three-domain moving nested simulation typhoon case, using ua and va inside the simulation results to synthesize the wind field, but I found that when using ua and va above the fifth layer level (top layer 50hpa, total 37 layers eta), , the inland high altitude wind speed of the typhoon is greater than the sea wind speed, which seems to be unreasonable, but the inland wind speeds in 10m wind field or low altitude wind field are smaller than the sea surfacewinds, which again makes perfect sense, has any researcher encountered a similar situation?