Variation of Air Temperature and Thermal Resources in the Northern and Southern Regions of the Qinling Mountains from 1951 to 2009

Expand
  • 1. Shaanxi Key Laboratory of Disaster Monitoring and Mechanism Modeling,Baoji University of Arts and Sciences 721013, Shaanxi, China;
    2. Institute of Geographic Sciences and Natural Resources Research, CAS, Beijing 100101, China;
    3. Graduate University of Chinese Academy of Sciences, Beijing 100049, China

Received date: 2011-06-09

  Revised date: 2011-07-11

  Online published: 2011-09-20

Supported by

Strategic Priority Research Program of the Chinese Academy of Sciences, No.XDA05090104; China Global Change Research Program. No.2010CB950903; Special Scientific Research Project for Public Interest, No. GYHY201106018;The National Natural Science Funds,No.41071359

Abstract

On the basis of daily air temperature data from 47 meteorological stations in the northern and southern regions of the Qinling Mountains (QLM) from 1951 to 2009, the variations of several criteria for temperature zones were analyzed including the mean annual temperature, the number of days with steady temperature above 10 ℃ and its accumulated temperature, the minimum temperature, mean temperatures during the coldest and hottest seasons. Our results show that climate warming in both northern and southern QLM was mainly observed after the 1990s, and the trends of mean annual temperature were consistent with the number of days with steady temperature above 10 ℃ and the accumulated temperature. Although these three indices showed a slight decline from 1951 to 1993 and a rapid increase since 1993, some seasonal and regional differences do exist. The average temperature of cold seasons of January exhibited the same changing trends with the minimum temperature, since they both slightly increased from 1951 to 1985 and declined since 1985. Meanwhile, the average temperature of hot seasons of July showed no significant trends. In addition, the increment of some indices showed differences among the northern areas to the QLM, southern slope of QLM, Hanshui River Basin and valleys in Daba and Wushan mountains. Compared with the period before 1993, the number of days with accumulated temperature steadily above 10 ℃ increased by 10, 10, 8 and 5 in the above four regions after 1993, accompanied by increments of related accumulated temperature by 278 ℃, 251 ℃, 235 ℃ and 207 ℃ respectively. Although the increment of thermal resources in the northern region of QLM had larger extent than that in the southern region, their variation trends were consistent and more marked in the cold season. Thus, the Qinling Mountains are still a boundary between the warm temperate zone and sub-tropical zone in China under the background of climate warming since the 1990s.

Cite this article

ZHOU Qi, BIAN Juanjuan, ZHENG Jingyun . Variation of Air Temperature and Thermal Resources in the Northern and Southern Regions of the Qinling Mountains from 1951 to 2009[J]. Acta Geographica Sinica, 2011 , 66(9) : 1211 -1218 . DOI: 10.11821/xb201109006

References

[1] Physical Geography in China Editorial Board of Chinese Academy of Sciences. Physical Geography in China: Introduction.Beijing: Science Press, 1985: 1-412. [中国科学院《中国自然地理》编辑委员会. 中国自然地理: 总论. 北京: 科学出版社,1985: 1-412.]

[2] Zhu Kezhen. Subtropics of China. Chinese Science Bulletin, 1958, 17: 524-527. [竺可桢. 中国的亚热带. 科学通报, 1958,17: 524-527.]

[3] Yang Qinye, Zheng Du, Wu Shaohong. On subtropical zone of China. Journal of Subtropical Resources and Environment,2006, 1(1): 1-10. [杨勤业, 郑度, 吴绍洪. 关于中国的亚热带. 亚热带资源与环境学报, 2006, 1(1): 1-10.]

[4] Kang Muyi, Zhu Yuan. Discussion and analysis on the geo-ecological boundary in Qinling Range. Acta Ecologica Sinica,2007, 27(7): 2774-2784. [康慕谊, 朱源. 秦岭山地生态分界线的论证. 生态学报, 2007, 27(7): 2774-2784.]

[5] Task Force on China's National Assessment Report on Climate Change. China's National Assessment Report on ClimateChange. Beijing: Science Press, 2007: 19-40. [《气候变化国家评估报告》编写委员会. 气候变化国家评估报告. 北京: 科学出版社, 2007: 19-40.]

[6] Ren Guoyu, Guo Jun, Xu Mingzhi et al. Climate changes of China's mainland over the past half century. ActaMeteorologica Sinica, 2005, 63(6): 942-956. [任国玉, 郭军, 徐铭志等. 近50 年中国地面气候变化基本特征. 气象学报,2005, 63(6): 942-956.]

[7] Sha Wanying, Shao Xuemei, Huang Mei. Climate warming and its impact on natural regional boundaries in China in the1980s. Science in China: Series D, 2002, 32(4): 317-326. [沙万英, 邵雪梅, 黄玫. 20 世纪80 年代以来中国的气候变暖及其对自然区域界线的影响. 中国科学: D辑, 2002, 32(4): 317-326.]

[8] Zhang Mingqing, Liu Guilian. The study on difference of spatial and temporal variation of air temperature in China and inlast 40 years. Meteorological Science and Technology, 1999 (1): 40-44. [张明庆, 刘桂莲. 我国近四十年气温变化时空差异研究. 气象科技, 1999, (1): 40-44.]

[9] Yan Junping, Zheng Yu. Acomparative study on environmental change response over the northern and the southern regionsof the Qinling Mountains. Geographical Research, 2001, 20 (5): 576-582. [延军平, 郑宇. 秦岭南北地区环境变化响应比较研究. 地理研究, 2001, 20(5): 576-582.]

[10] Miao Qilong, Ding Yuanyuan, Wang Yong. Impact of climate warming on the northern boundary of subtropical zone ofChina. Geographical Research, 2009, 28(3): 634-642. [缪启龙, 丁园圆, 王勇. 气候变暖对中国亚热带北界位置的影响.地理研究, 2009, 28(3): 634-642.]

[11] Ding Min, Huang Chunchang. The influence of climatic warming on fruit produce in northern foot of Qinling Mountain.Journal of Natural Resources, 2003, 18(2): 235-239. [丁敏, 黄春长. 秦岭北麓平原对全球变暖的响应及其对果业发展的影响研究. 自然资源学报, 2003, 18(2): 235-239.]

[12] Chen Xianji. A new approach to the climate division of China. Acta Meteorologica Sinica, 1982, 40(1): 35-47. [陈咸吉. 中国气候区划新探. 气象学报, 1982, 40(1): 35-47.]

[13] Physical Geography in China Editorial Board of Chinese Academy of Sciences. Physical Geography in China:Climatology. Beijing: Science Press, 1985: 1-161. [中国科学院《中国自然地理》编辑委员会. 中国自然地理:气候. 北京: 科学出版社, 1985: 1-161.]
Outlines

/