The Motooka district located in the northern part of Kyushu is scheduled to be the new campus of Kyushu University in near future. The area of about 250ha shall be greatly changed from full vegetation and full of ups and downs of mountain to less vegetation and partly flat with many buildings. We focus our thoughts on meteorological change which is brought by such big development, and the assessment is not only important for the University itself, but also for the global environment problems. The observations, therefore, were conducted for the present actual situation before development of the land, and comparisons of data of Motooka with the fully urbanized area of Fukuoka and the urbanizing area of Maebaru as bedtown of Fukuoka were also done. The results for the summer of 1994, which recorded extremely high and dry, and the winter of 1994-1995 were summarized as follows; 1. The daily maximum air temperature in Motooka was between Fukuoka and Maebaru in summer, and Motooka was nearly equal with Fukuoka but higher than Maebaru in winter. 2. On the daily minimum airtemperature, Motooka was 3.7℃ and 2.0℃ lower than Fukuoka and Maebaru respectively in summer, and was lower 2.4℃ and 0.8℃ than Fukuoka and Maebaru respectively in winter. The occurrence number of the tropical night (≧25℃) in Motooka was only 3 days in contrast with 50 days in Fukuoka and 25 days in Maebaru. The reason was thought to be the difference in vegetation, degree of urbanization and wind speed. 3. On the daily mean air temperature, Motooka was substantially lower than Fukuoka and Maebaru both in summer and winter. 4. On the diurnal range of air temperature, Motooka was larger than Fukuoka and Maebaru in both summer and winter. Those difference among the locations enlarged on fair days. 5. On the humidity, Motooka was more moist than Fukuoka and Maebaru in both summer and winter. The vegetation in mountainside and in farm kept humidity higher, and vegetation less in urban area should cause heat-island phenomena. 6. Wind speed in Motooka showed diurna1 change, strong in the daytime and weak at night, but these values were substantially weaker than those of Fukuoka. This fact effected the difference in air temperature among the area. 7. Main wind direction in Motooka were ruled by the topographical feature in both summer and winter, that is, southwesterly and northeasterly winds along with valley. Those of Fukuoka were northwesterly and southeasterly winds in both summer and winter, which is effected by sea-breeze and land-breeze.