1994 年 59 巻 462 号 p. 49-58
The data not only in a downward looking mode but also in north- and south-side looking modes by using airborne MSS at noon on a winter clear sky day have been obtained to clarify the radiant temperature distribution over observed area by taking account of unevenness of the area. Based on observed data and GIS data, sensible heat flux from the overall surface to air at each developed area was calculated, which is considered as a main factor in determining air temperature. Moreover, the relationships between land coverage conditions and amount of sensible heat flux were analyzed.