西安地区土壤浅层温度变化特征
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  • 英文篇名:Characteristics of shallow soil temperature changes in Xi’an area
  • 作者:刘引鸽 ; 周欢欢 ; 胡浩楠 ; 方建刚 ; 龙颜
  • 英文作者:LIU Yinge;ZHOU Huanhuan;HU Haonan;FANG Jiangang;LONG Yan;College of Geography and Environment,Baoji University of Arts and Sciences;Key Laboratory of Disaster Monitoring and Mechanism Simulating of Shaanxi Province,Baoji University of Arts and Sciences;Shaanxi Provincial Climate Center;
  • 关键词:地温 ; 时空特征 ; 影响因素 ; 西安地区
  • 英文关键词:ground temperature;;trend,chronological characteristics;;Xi'an area
  • 中文刊名:GHZH
  • 英文刊名:Journal of Arid Land Resources and Environment
  • 机构:宝鸡文理学院地理与环境学院;宝鸡文理学院陕西省灾害监测与机理模拟重点实验室;陕西省气候中心;
  • 出版日期:2019-05-30
  • 出版单位:干旱区资源与环境
  • 年:2019
  • 期:v.33;No.252
  • 基金:国家自然科学基金项目(41771048);; 国家社会科学基金项目(15XZZ012);; 陕西省教育厅计划项目(13JS010);; 宝鸡文理学院重点项目(ZK16061);宝鸡文理学院自然地理学陕西省重点学科基金项目资助
  • 语种:中文;
  • 页:GHZH201908021
  • 页数:7
  • CN:08
  • ISSN:15-1112/N
  • 分类号:155-161
摘要
利用西安地区1961-2017年的逐月5、10、15、20cm浅层地温观测数据,采用气候诊断方法,研究了西安地区土壤浅层温度的时间变化趋势,以及地温随土层深度的变化特征,探讨了影响地温变化因素。结果表明:西安地区各浅层年季平均地温有显著上升趋势,以郊区地温变化率最大,城区地温变化率较小,地温随土层深度变化有差异。土层越深,趋势率越小,春夏两季地温随土层深度增加而下降,秋冬两季土层深度越深而地温越高。同时也检测出地温具有周期、突变及异常特征。分析认为气温升高是影响地温变化的主要因素,下垫面性质及地热传导与地温的空间变化有密切关系。
        Based on the 5, 10, 15 and 20 cm shallow ground temperature observation data of four meteorological observation stations in Xi'an from 1961 to 2017, using climate tendency rate, MK test and wavelet analysis methods, the trends, mutation characteristics, abnormal years and periodic characteristics of shallow ground temperature were analyzed. The results show that the annual average shallow ground temperature of 5, 10, 15 and 20 cm in Xi'an area were increasing significantly with the increase of soil depth in the vertical direction. The ground temperature in spring and summer decreased with the increase of soil depth, but were increasing with the increase of soil depth in autumn and winter. At the same time, the ground temperature showed periodicity, mutation and abnormal characteristics. The analysis shows that the temperature, underlying surface properties and geothermal conduction had a great influence on the ground temperature.
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