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Air temperature, soil temperature, humidity, wind speed and wind direction were observed at the sloped and lowland areas of the Turfan Basin from Nov. 26 to 28, 1991 and the characteistics of inversion layer, cold air current and temperature resources were made clear as follows (1) Profiles of air temperature and relative humidity showed symmetrical changing patterns. Occurrence rate and intensity of temperature inversion were high in an early morning under weak wind on clear-fine day in winter. Averaged daily maximum and minimum gradients were 0.8•Ž/ m and temperature inversion of -2.0•Ž/m, respectively in winter. Vertical profiles of wind speed expressed stable or unstable patterns shifted from the log-low profile. (2) Air temperature increases with the increaseof wind speed in night and vice versa. The changing pattern of 3 hour cycle was observed at the Turfan Desert Research Station of -80 m in a lowland area of the basin. (3) The higher inversion layer and trailing smoke were observed at the level of about 500 in and not destroyed even in the daytime. (4) The temperature diffence of inversion between the sloped area and lowland area near the basin bottom was 2•Ž at noon, 4•Žat night and 8•Ž in an early morning, and temperature resources of thermal belt seem to be useful. 1992年7月5日 全 国大会 にて発表 1994年5月19日 受付',1994年12月9日 受理

Characteristics on Air Temperature and Humidities of Inversion Layer and Wind in Winter at Turfan Basin.