中国农业气象 ›› 2011, Vol. 32 ›› Issue (增刊): 1-4.

• 论文 •    下一篇

近49年德州浅层地温的变化特征分析

代玉田,裴洪芹,杨玉霞   

  1. 德州市气象局,德州 253078;临沂市气象局,临沂 276004
  • 出版日期:2011-10-31 发布日期:2011-11-24

Variation Analysis of Shallow Geothermal of Dezhou City in Nearly 49 Years

DAI Yu tian,PEI Hong qin,YANG Yu xia   

  1. Dezhou Meteorological Bureau of Shandong Province, Dezhou 253078,China;Linyi Meteorological Bureau of Shandong Province, Linyi 276004
  • Online:2011-10-31 Published:2011-11-24

摘要: 采用德州气象站1961-2009年0-20cm各层逐月平均地温、降水量和平均气温,研究了近49a德州浅层平均地温的变化特征及与降水和气温的关系。用九点二次平滑技术来滤除要素序列的年代际变化趋势。结果表明:〖JP2〗浅层各季节平均地温均呈升高趋势,升温速率为0.22~0.485℃/10a,春季和秋季最大,夏季最小;各层年平均地温20世纪60年代-90年代中期为偏冷阶段,90年代中后期至今为偏暖阶段;气温升高及降水减少是影响地温上升的主要原因。〖JP3〗研究结果对于合理利用气候资源,适当调整种植区划和合理安排农业生产布局具有参考价值。

关键词: 浅层地温, 气候倾向率, 地温异常

Abstract: By using monthly mean geothermal, precipitation and mean temperature of the depth of 0-20cm during 1961 to 2009 at Dezhou meteorological station, the variation of average shallow geothermal and the relationship between geothermal and precipitation as well as mean temperature were analyzed. The decadal variation of sequence elements is filtered with 9.2 times of smoothing techniques, demonstrating the trend. The results showed that the mean shallow geothermal in each season increased with the rate of 0.22~0.485℃ per 10 years, maximum in spring and autumn, minimum in summer. Annual mean shallow geothermal in each layer from 1960s to the middle of 1990s was the cold periods, and in the late 1990s was the warm period. The main reasons of impact on geothermal increasing were the increasing temperature and the decreasing precipitation. The results could provide a reference to utilizing climatic resources and adjusting planting division and distribution of agricultural production.

Key words: Shallow geothermal, Climate trend rate, Geothermal abnormal