摘要
In this study, we analyzed the changes of houdy temperature in some regions of Guanzhong Plain in the north of Qingling Mountains on December 4, 2012. The results show that daily variation of temperature was abnormal in some regions of Guanzhong Plain on December 4, 2012, and medium fog and haze inhibited the increase of air temperature in the urban area of Xi＇an in the morning of December 4, so that air temperature went up slowly during the day of December 4. The sinking of the northwest cold air before arriving Guanzhong Plain as well as atmospheric com- pression warming effect caused by Qinling terrain blocking were the main reasons for the abnormal increase of temperature in some areas of Guanzhong Plain. Compared with surrounding districts and counties, urban heat island effect was more obvious in the urban area of Xi＇an.
In this study, we analyzed the changes of houdy temperature in some regions of Guanzhong Plain in the north of Qingling Mountains on December 4, 2012. The results show that daily variation of temperature was abnormal in some regions of Guanzhong Plain on December 4, 2012, and medium fog and haze inhibited the increase of air temperature in the urban area of Xi＇an in the morning of December 4, so that air temperature went up slowly during the day of December 4. The sinking of the northwest cold air before arriving Guanzhong Plain as well as atmospheric com- pression warming effect caused by Qinling terrain blocking were the main reasons for the abnormal increase of temperature in some areas of Guanzhong Plain. Compared with surrounding districts and counties, urban heat island effect was more obvious in the urban area of Xi＇an.
基金
Supported by the Special Project for Forecasters of Shaanxi Meteorological Bureau in 2013 (2013Y-17)
Key Scientific Research Projectof Shaanxi Province (2013Z-3)
