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Arid Land Geography ›› 2020, Vol. 43 ›› Issue (4): 977-996.doi: 10.12118/j.issn.1000-6060.2020.04.13

• Climatology and Hydrology • Previous Articles     Next Articles

Characteristics of specific humidity distribution and profiles in Urumqi City and suburbs

LI Zhen-jie1,2,3, JIN Li-li4,5, HE Qing4,5, MIAO Qi-long5, ALI Mamtimin4   

  1. 1 Lincang Meteorological Bureau,Lincang 677099,Yunnan,China;
    2 Xinjiang Institute of Ecology and Geography,Chinese Academy of Sciences,Urumqi 830011,Xinjiang,China;
    3 University of Chinese Academy of Sciences,Beijing 100049,China;
    4 Taklimakan Desert Meteorology Field Experiment station of CMA,Institute of Desert Meteorology,China Meteorological Administration,Urumqi 830002,Xinjiang,China;
    5 College of Applied Meteorology,Nanjing University of Information Science and Technology,Nanjing 210044,Jiangsu,China
  • Received:2019-07-05 Revised:2020-03-15 Online:2020-07-25 Published:2020-11-18

Abstract: Observations from L-Band radar and 10-layer data collected at five 100-m-high meteorological towers in Urumqi City,Xinjiang,northwestern China were used to analyze the characteristics of the specific-humidity profile within 2 km,including seasonal and diurnal variation in urban and suburban Urumqi. The results,which reveal moisture inversion,were as follows:(1) The levels of specific humidity vary by season (summer>autumn>spring>winter). In summer,specific humidity is about 4-5 times that of winter,and that of autumn is ~1 g ·kg-1 more than in spring. In spring,summer,and autumn,the specific humidity was less at greater heights,especially in summer,whereas the change with height was less in winter. Multiple minimum values appeared on the specific humidity profile,and the appearance height is basically the same. The daily variation of specific humidity was the most in summer and winter but opposite in phase during these seasons. The specific humidity is high (low) at night,low (high) during the day in summer (winter). Specific humidity is less in the suburbs than in urban areas in winter,but it is the urban-suburban difference is less obvious in the other seasons. (2) Moisture inversion is evident within 2 km. Its probability is>35%. January shows the maximum probability,and July,the minimum. In January,the maximum height of moisture inversion is>1 500 m,but in July it can reach 1 900 m,with a maximum thickness of<1 550 m. The maximum moisture inversion was 2.5 g·kg-1 per 100 m in July and October,and the minimum was in January. (3) Moisture inversion often was accompanied by temperature inversion in January in Urumqi. The vertical distribution of water vapor changed according to the temperature-inversion layers. The moisture inversion,which is also related to water-vapor transport,usually appeared from the top of the temperature-inversion layer. This study can effectively reveal seasonal characteristics of air humidity and provide a basis for studying meteorological factors affecting air pollution in cities.

Key words: boundary layer, specific humidity, profile, Urumqi City