To analyze the relationship between outgoing longwave radiation (OLR) and cyclogenesis, we visualized the strong typhoon period during Sep 17th through the 28th in 1999. Using CMIP5 and CanESM2 data sets, it forced as boundary forcing value to WRF for 10 years integration from 1990. We defined new variable "wind speed" by horizontal, meridional, and vertical wind and visualized in 3-D utilizing the DVR method of VAPOR. In addition, the appearance of "wind speed" is treated by isosurface appearance method of VAPOR to show the air temperature change in altitude. OLR was extracted only the value which relate with cyclogenesis and was shown the heat flux transportation from the ocean to atmosphere.
