论文

川渝地区气候与物候的变化特征分析

展开
  • 成都信息工程学院 高原大气与环境四川省重点实验室 大气科学学院, 四川 成都 610225

收稿日期: 2010-08-10

  修回日期: 2010-10-10

  网络出版日期: 2011-06-20

基金资助

国家自然科学基金项目(40875053)、局校合作项目"西藏近40年植被物候资料恢复重建研究"共同资助。

Climate and Phenology Variations in Sichuan and Chongqing

Expand
  • Plateau Atmosphere and Environment Key Laboratory of Sichuan Province, College of Atmospheric Sciences, Chengdu University of Information technology, Chengdu, Sichuan 610225, China

Received date: 2010-08-10

  Revised date: 2010-10-10

  Online published: 2011-06-20

摘要

利用川渝地区44个气象台站的气象资料和2个物候观测站的物候资料分析了该地区的气候与物候变化特征:最近10 a年均温度比前30多a高0.68℃,年均降水量基本无变化。低温主要分布在川西高原,低温天数、低温积温绝对值都在减少。日均最高温度在高原南部、西南山地减少,其它地区都增加;日均最低温度都在增暖。降水在四川盆地下降,在重庆西部、川西高原增加。降水日数在高原西部增加,其它地区都下降。春始期仁寿略微推迟,北碚微弱提前;秋始期都推迟。展叶期的杏树、刺槐、水杉、紫荆、梧桐推迟,紫藤、毛桃提前。落叶期仁寿刺槐提前,北碚的植物全部推迟。

本文引用格式

王炳赟, 范广洲, 董一平, 华维, 周定文, 朱丽华, 张琪 . 川渝地区气候与物候的变化特征分析[J]. 地理科学, 2011 , 31(6) : 674 -681 . DOI: 10.13249/j.cnki.sgs.2011.06.674

Abstract

According to the daily temperature and precipitation data of 44 stations in 1961-2007 and part of the woody plant data of Beibei observation stations and Renshou observation stations in 1963-1988, the Chinese Academy of phenological observation network in Sichuan-Chongqing, temperature, precipitation, season, woody plant phenology variation were analyzed. The results showed that mean annual temperature of the last 10 years were 0.68 ℃ higher than the previous 37 years, and mean annual precipitation basically unchanged. Low temperature is mainly distributed in the western Sichuan Plateau, and the number of low temperature days and accumulated low temperature decreased. Mean daily maximum temperature in the southern region of the western Sichuan Plateau tended to decrease, while that in other regions increased. Mean daily minimum temperature was confirmed to have warming trends, and that in the southwestern Sichuan and the northern Sichuan Plateau grew faster. Precipitation in the central and southern of Sichuan Basin declined, southwest of Chongqing and western Sichuan plateau tended to increase. Precipitation days in the western Sichuan Plateau demonstrated an increasing trend, that in other regions tended to decrease, especially, those decreased rapidly in the east of Sichuan and Chongqing. According to Zhang Baokun Designate Temperature Method to define seasons, spring starting time delayed in Renshou, advanced in Beibei, and autumn starting time delayed in those two stations. In the leaf expansion phase, apricot and black locust of Renshou, and black locust, Metasequoia, Bauhinia, Indus of Beibei delayed, wisteria, peaches of Beibei advanced. In the leaf defoliation stage, black locust of Renshou advanced, but all plants of Beibei delayed.

参考文献

[1] Intergovernmental Panel on Climate Change. Climate Change 2007: The physical science basis[C]//Contribution of Working Group 1 to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change. Cambridge: Cambridge University Press, 2007.
[2] Mann M E,Bradley R S,Hughes M K.Northern Hemisphere temperature during the past Millennium: Inferences, Uncertainties and Limitations[J]. Geophysical Research Letters,1999,26(6): 759-762.
[3] 丁一汇,戴晓苏.中国近百年(1860~1990年)来的温度变化[J].气象,1994,20(12):19~26.
[4] 王翠花,李雄,缪启龙.中国近50年来日最低气温变化特征研究[J].地理科学,2003,23(4):441~447.
[5] 郭志梅,缪启龙,李 雄.中国北方地区近50年来气温变化特征的研究[J].地理科学,2005,25(4):448~454.
[6] 左洪超,吕世华,胡隐樵.中国近50年气温及降水量的变化趋势分析[J]. 高原气象,2004,23(2):238~244.
[7] 刘学华,季致建,吴洪宝,等.中国近40年极端气温和降水的分布特征及年代际差异[J].热带气象学报,2006,22(6):618~624.
[8] 张福春.气候变化对中国木本植物物候的可能影响[J].地理学报,1995,50(5):402~410.
[9] 葛全胜,郑景云,张学霞,等.过去40年中国气候与物候的变化研究[J].自然科学进展,2003,13(10):1048~1053.
[10] 徐文铎,邹春静,卜 军.全球变暖对中国东北植被的影响及对策[J].地理科学,1996,16(1):26~36.
[11] 陈效逑,李 倞.内蒙古草原羊草物候与气象因子的关系[J].生态学报,2009,29(10) :5280~5290.
[12] 陆佩玲,于 强,贺庆棠.植物物候对气候变化的响应[J].生态学报,2006,26(3):923~929.
[13] 王传海,吴飞倩,李淑娟,等.西安植物园木本植物近十余年物候变化的特征分析[J].中国农业气象,2006,27(4):261~264.
[14] 中国气象局预测减灾司,中国气象局国家气象中心.中国气象地理区划手册[M].北京:气象出版社,2006:48~51.
[15] 马柱国,符涂斌,任小波,等.中国北方年极端温度的变化趋势与区域增暖的联系[J].地理学报,2003,58(Supplement):11~20.
[16] 王 菱,谢贤群,苏 文,等.中国北方地区50年来最高和最低气温变化及其影响[J].自然资源学报,2004,19(3):337~343.
[17] Easterling D R, J L Evans, P Ya Groisuran, et al. Observed variability and trends in extreme climate events: a brief review Bull. of the Ameri. Mete[J]. Soci., 2000,81(3): 417-425.
[18] 张宝堃.中国季节之分布[J].地理学报,1934,1(1):1~18.
[19] 郑景云,葛全胜,郝志新,等.气候增暖对我国近40年植物物候变化的影响[J].科学通报,2002,47(20):1582~1587.
[20] 张 杰,李栋梁,王 文.夏季风期间青藏高原地形对降水的影响[J].地理科学,2008,28(2):236~240.
[21] 郑景云,葛全胜,赵会霞,等.近40年中国植物物候对气候变化的响应研究[J].中国农业气象,2003,24(1):28~32.
[22] 李洪权,范广洲,周定文,等.青藏高原春季植被变化特征及其对夏季气温的影响[J].地理科学,2008,28(2):259~265.
[23] 徐雨晴,陆佩玲,于 强.近50年北京数据物候对气候变化的响应[J].地理研究,2005,24(3):412~420.
[24] 李国平,肖 杰.青藏高原西部地面反射率的日变化以及与若干气象因子的关系[J].地理科学,2007,27(1):63~67.
[25] 何云玲,张一平,杨小波.中国内陆热带地区近40年气候变化特征[J].地理科学,2007,27(4):499~505.
[26] 陈效逑.论树木物候生长季节与气温生长季节的关系——以德国中部Taunus山区为例[J].气象学报,2000,58(6):726~737.
[27] 房巧敏,龚道溢,毛 睿.中国近46年来冬半年日降水变化特征分析[J].地理科学,2007,27(5):711~717.
文章导航

/