Notice of RetractionAnalysis to atmospheric boundary sounding of a sea fog process on Donghai island of Zhanjiang

Notice of Retraction

After careful and considered review of the content of this paper by a duly constituted expert committee, this paper has been found to be in violation of IEEE´s Publication Principles.

We hereby retract the content of this paper. Reasonable effort should be made to remove all past references to this paper.

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The temperature is superadiabatic degressive at 70 meters below, and is approximate isothermal at 70-120 meters during fog process. The temperature inversion occurs apparently at night because that wind direction turns clockwise with high so that there is warming advection in boundary. In fog process, relative humidity increases with high in detection area and exceeds 85% above 80 meters, above of which increases relatively slowly . Relative humidity contour approximate exponentially distributed under 120 meter. Wind speed exceeds 10 meters per second above 120 meters height at boundary and linearly increases with height. Wind profiling has an approximate linear distribution at detection range during fog process. Wind direction is basically unchanged with high above 20 meters, which is the basic easterly wind or southeast wind so that it brings moisture vapor from the sea. Wind direction turns clockwise with high which led directly to the phenomenon of the atmospheric warming significantly at night.