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中国农学通报 ›› 2015, Vol. 31 ›› Issue (29): 221-226.doi: 10.11924/j.issn.1000-6850.casb15050117

所属专题: 农业气象

• 资源 环境 生态 土壤 气象 • 上一篇    下一篇

辽宁省近56年来气温变化研究

薛双奕,杨东,马露   

  1. 西北师范大学地理与环境科学学院,西北师范大学地理与环境科学学院,西北师范大学地理与环境科学学院
  • 收稿日期:2015-05-21 修回日期:2015-06-30 接受日期:2015-07-24 出版日期:2015-10-28 发布日期:2015-10-28
  • 通讯作者: 薛双奕
  • 基金资助:
    国家自然科学基金“甘肃窑街侏罗纪真蕨植物化石微细构造”(41262001)

Study on Temperature Changes in Recent 56 Years in Liaoning Province

  • Received:2015-05-21 Revised:2015-06-30 Accepted:2015-07-24 Online:2015-10-28 Published:2015-10-28

摘要: 为了简单分析辽宁省气温变化的现状,根据辽宁省23 个气象站点1958—2013 年的年平均气温、平均最高气温、平均最低气温以及极端最高、极端最低气温等气象要素资料,通过气候倾向率、滑动平均、Mann-Kendall 突变检验以及反距离权重插值法等方法,分析了辽宁省近56 年来气温变化的特征。结果表明:辽宁省年均气温整体呈明显的上升的趋势,尤其是20世纪90年代后,年均气温的增加趋势更加显著。受纬度及海陆位置差异等因素的影响,辽宁省年均气温的空间分布整体上是由东北向西南方向逐渐增强。在整个时间域内年均气温波动存在1 个突变点,即发生在1988 年;并且主要存在3 个主周期,第1主周期为12年,第2、3主周期为21~22年和8年,各主周期都有一定的年代际变化。

关键词: 农村居民点, 农村居民点, 分布特征, GIS, 醴陵市

Abstract: The paper aims to analyze the current situation of temperature changes in Liaoning Province.According to the meteorological data, such as annual average temperature, average maximum temperature, average minimum temperature and extreme maximum and extreme minimum temperature from 23 meteorological stations in 1958 to 2013 in Liaoning Province, The authors adopted the methods such as the climate tendency rate, moving average, Mann- Kendall mutation test and the inverse distance weighted interpolation (IDW) to analyze the characteristics of temperature change in recent 56 years in Liaoning Province. The results showed that the average annual temperature of Liaoning Province had an obvious rising trend on the whole, especially after 1990s, the increase of the average annual temperature trend was more significant. Affected by the latitude and the location of the land and sea differences and other factors, the spatial distribution of annual average temperature of Liaoning Province was gradually enhanced from northeast to southwest. In the whole time domain, average annual temperature fluctuations had a point mutation, which happened in 1988. And there were 3 main cycles, the first main cycle was for 12 a, the second and the third main cycle were for 21-22 a and 8 a respectively, all the main cycles had certain decadal variability.