Abstract
The cool-island phenomena were observed at Osaka Castle Park on August 1-15, 2007. The surface-air temperature inside the park was nocturnally lower than that around urban areas. The cool-island intensity was more than +2.0°C during 4–5 JST. The cooler air generated inside the park extended downwind at the distance of about 250 m. Next, we compared the atmospheric cooling amounts on the forest area with that on the lawn area. As a result, it was suggested that the cooler air over the forest canopy subsided into and accumulated on the ground surface.