[1]赵 军,黄永生,师银芳,等.2000—2012年祁连山中段雪线变化与气候变化关系[J].山地学报,2015,(06):683-689.[doi:10.16089/j.cnki.1008-2786.000082]
 ZHAO Jun,HUANG Yongsheng,SHI Yinfang,et al.Relationship Between Sonw Line Change and Climate Changein the Middle of Qilian Mountains during 2000—2012[J].Mountain Research,2015,(06):683-689.[doi:10.16089/j.cnki.1008-2786.000082]
点击复制

2000—2012年祁连山中段雪线变化与气候变化关系()
分享到:

《山地学报》[ISSN:1008-2186/CN:51-1516]

卷:
期数:
2015年06期
页码:
683-689
栏目:
山地生态与环境
出版日期:
2015-12-01

文章信息/Info

Title:
Relationship Between Sonw Line Change and Climate Change in the Middle of Qilian Mountains during 2000—2012
作者:
赵 军黄永生师银芳李 龙
西北师范大学地理与环境科学学院,甘肃 兰州 730070
Author(s):
ZHAO Jun HUANG Yongsheng SHI Yinfang LI Long
College of geographic and Environmental Science, Northwest Normal University, Lanzhou 730070, China
关键词:
祁连山 雪线 气候变化 MOD10A2
分类号:
P467
DOI:
10.16089/j.cnki.1008-2786.000082
文献标志码:
A
摘要:
利用MOD10A2积雪产品、气温、降水数据和DEM数据,借助于GIS空间分析技术和统计方法,分析2000—2012年祁连山中段地区的雪线变化,并探讨温度和降水对雪线变化的影响。研究结果表明:1. 2000—2012年祁连山中段雪线平均高程值呈波动上升,平均上升速率为42.3 m/(10 a); 各年的雪线平均高程>4 600 m,多年雪线平均高程值为4 673 m。2.祁连山中段地区各坡向的雪线平均高程值、年平均上升速率均呈现相一致的特征,即阳坡>半阴半阳坡>阴坡。3. 2000—2012年暖季气温和6—8月累计降水量是影响祁连山雪线变化的重要因素,暖季气温升高是引起雪线升高的主导因素。在6—8月累计降水量保持稳定的情况下,暖季气温上升(下降)1℃,祁连山中段雪线高度上升(下降)约58 m。

参考文献/References:

[1] Wang Shaowu. Snow covered and climate change [J]. Geographical Research,1983,2(3):73-86 [王绍武.冰雪覆盖与气候变化[J].地理研究,1983,2(3):73-86]
[2] Kalesnik. Overview of glaciology[M].Lanzhou: Cold and Arid Regions Environment al and Engineering Research Institute, Chinese Academy of Science, 1982:28-40 [卡列斯尼克.冰川学概论[M].兰州:中国科学院兰州冰川冻土研究所,1982:28-40]
[3] Deng Yuwu, Xie Zichu, Li Lingling. Creating the distribution field of equilibrium line altitude based on GIS in the southen of TIBET and analyzing its distribution characters [J].Yun Nan geographic environment research. 2006,3:10-14 [邓育武,谢自楚,李玲玲.基于GIS的西藏南部雪线场的建立及其空间分布特征[J].云南地理环境研究,2006,310-14]
[4] Jung Fuchu, Wu Xihao, Wang Shubing, et al. Characteristics of space distribution of the climate snowline in China [J]. Journal of Geomechanics,2002,4:289-296 [蒋复初,吴锡浩,王书兵,等.中国气候雪线空间分布特征[J].地质力学学报,2002,4:289-296]
[5] Jiang Zhongxin. Trend surface analysis of the existent snowline in West China. Chinese Geographical Science, 1991, 1(1): 62-69
[6] Li Jijun, Zheng Benxing, Yang Xijin, et al. Glacier of Tibet[M].Beijing: Science Press, 1986,28-30 [李吉均,郑本兴,杨锡金,等.西藏冰川[M].北京:科学出版社,1986,28-30]
[7] Shi Yafeng. Overview of Chinese Glaciology [M]. Beijing: Science Press, 1988:15-18 [施雅风.中国冰川概论[M].北京:科学出版社,1988:15-18]
[8] Shi Yafeng, Shen Yongping, Hu Ruji. Preliminary study on signal, impact and foreground of climatic shift from warm-dry to warm-humid in Northwest China [J]. Journal of Glaciology and Geocryology,2002,3:219-226 [施雅风,沈永平,胡汝骥.西北气候由暖干向暖湿转型的信号、影响和前景初步探讨[J].冰川冻土,2002,3:219-226]
[9] Qin Dahe, Ding Yihui, Su Jilan, et al. Assessment of climate environment Climate and environment changes in China(I): Climate and environment changes in China and their projection [J]. Advances in Climate Change Research, 2005,1(1):4-9 [秦大河,丁一汇,苏纪兰,等.中国气候与环境演变评估(I):中国气候与环境变化及未来趋势[J].气候变化研究进展,2005,1(1):4-9]
[10] Chen Qian, Chen Tianyu. Climatical analysis of seasonal snow resources in Qilian MT[J].Geographical Research,1991,10(1):24-38 [陈乾,陈添宇.祁连山区季节性积雪资源的气候分析[J].地理研究,1991,10(1):24-38]
[11] Zhang Jie, Han Tao, Wang Jian. Snow area and snow line altitude change in Qilian Mountains from 1997 to 2004 [J]. Journal of Glaciology and Geocryology,2005, 27(5):649-654 [张杰,韩涛,王建.祁连山区1997-2004年积雪面积和雪线高度变化分析[J].冰川冻土,2005, 27(5):649-654]
[12] Cai Dihua, Guo Ni, Wang Xing, et al. The Spatial and Temporal Variations of Snow Cover over the Qilian Mountains based on MODIS Data[J].Journal of Glaciology and Geocryology,2009,31(6):1028-1036 [蔡迪花,郭铌,王兴,等.基于MODIS的祁连山区积雪时空变化特征[J]. 冰川冻土,2009,31(6):1028-1036]
[13] Xiao Fei, Du Geng, Ling Feng, et al. Digital Extraction of Snowline based on Flow Path Analysis[J]. Journal of RemoteSensing,2010,14(1):55-67 [肖飞,杜耘,凌峰,等.基于水流路径分析的雪线数字提取[J]. 遥感学报,2010, 14(1):55-67]
[14] Hao Xiaohua, Wang Jian, Li Hongyi. Evaluation of the NDSI threshold value in mapping snow cover of MODIS: A case study of snow in the middle Qilian Mountains [J]. Journal of Glaciology and Geocryology,2008, 30(1):132-138 [郝晓华,王建,李弘毅. MODIS雪盖制图中NDSI阈值的检验[J].冰川冻土,2008,30(1):132-138]
[15] Li Sanmei, Yan Hua, Liu Cheng. Study of snow detection using FY-2C Satellite Data[J].Journal of Remote Sensing,2007,11(3):406-413 [李三妹,闻华,刘诚.FY-2C积雪判识方法研究[J].遥感学报,2007,11(3): 406-413]
[16] Yan Hao, Zhang Guoping. Unmixing Method applied to snow boundary estimation [J]. Mountain Research,2004,22(1):110 -115[延昊,张国平.像元分解法提取积雪边界线[J].山地学报,2004,22(1):110 -115]
[17] Wang Xing. The Characteristics Research of Satellite-Based Remote Sensing of Snow Qilian Area [D].Masters Degree Thesis, Beijing: Chinese Academy of Meteorological Sciences, 2008:1-3 [王兴.基于卫星遥感的祁连山区积雪特征研究[D].北京:中国气象科学研究院,2008:1-3]
[18] Tian Hongzhen,Yang Taibao,Liu Qinping.Climate change and glacier retreat in Ganggeexiaoheli,middle Qilian Mountains using remote sensing data,1976-2010[J].Journal of Arid Land Resources and Environment,2012,7:41-46[田洪阵,杨太保,刘沁萍.1976-2010年祁连山中段岗格尔肖合力雪山冰川退缩和气候变化的关系研究[J].干旱区资源与环境,2012,7:41-46]
[19] Pu Jianchen, Yao Tandong, Duan Keqin, et al. Mass balance of the Qiyi Glacier in the Qilian Mountains:a new observation [J]. Journal of Glaciology and Geocryology,2005,27(2):199-204 [蒲健辰,姚檀栋,段克勤,等.祁连山七一冰川物质平衡的最新观测结果[J].冰川冻土, 2005,27(2):199-204]
[20] Gao Qianzhao, Yang Xinyuan. The Features of interior Rivers and Feeding of Glacial Melt-water in the Hexi Region, Gansu Province[G]//Memoirs of Lanzhou institute of glaci ology and cryopedology Chinese academy of science, No.5.Beijing: Sciences Press,May,1992. [高前兆,杨新源.甘肃河西内陆河径流特征与冰川补给[G]//中国科学院兰州冰川冻土研究所集刊,第5号.北京:科学出版社,1992.]
[21] Wang Ninglian, He Jianqiao, Pu Jianchen, et al. Variations in equilibrium line altitude of the Qiyi Glacier, Qilian Mountains, over the past 50 years [J]. Chinese Science Bulletin, 2010, 55(32): 3107-3115 [王宁练,贺建桥,蒲健辰,等.近50年来祁连山七一冰川平衡线高度变化研究[J].科学通报,2010,55(32): 3107-3115]
[22] Chen An'an, Chen Wei, Wu Hongbo, et al. The variations of firn line altitude on the Binglinchuan Glacier, Ulugh Muztagh during 2000—2013 [J]. Journal of Glaciology and Geocryology,2014,36(5):1069-1078 [陈安安,陈伟,吴红波,等.2000—2013年木孜塔格冰鳞川冰川粒雪线高度变化研究[J].冰川冻土,2014, 36(5):1069-1078]

相似文献/References:

[1]周万福,肖宏斌,孙安平,等.祁连地形云与垂直风的关系[J].山地学报,2012,(06):641.
 ZHOU Wanfu,XIAO Hongbin,SUN Anping,et al.The Relation between Orographic Cloud and  Vertical Wind in Qilian[J].Mountain Research,2012,(06):641.
[2]赵成章,董小刚,石福习,等.高寒山区退耕地不同植被恢复方式下群落稳定性[J].山地学报,2011,(01):6.
 ZHAO Chengzhang,DONG Xiaogang,SHI Fuxi,et al.Community Stability under Different Vegetations Restored of Abandoned Lands in Alpine Areas[J].Mountain Research,2011,(06):6.
[3]赵井东,周尚哲,崔建新,等.摆浪河流域的ESR年代学与祁连山第四纪冰期新认识[J].山地学报,2001,(06):481.
[4]张虎,温娅丽,马力,等.祁连山北坡中部气候特征及垂直气候带的划分[J].山地学报,2001,(06):497.
[5]牛云,张宏斌,刘贤德,等.祁连山主要植被下土壤水的时空动态变化特征[J].山地学报,2002,(06):723.
[6]胡启武,欧阳华,刘贤德,等.祁连山北坡垂直带土壤碳氮分布特征[J].山地学报,2006,(06):654.
[7]罗永忠,郭小芹*,刘绪珍.1961-2013年气候变化对祁连山草地生产力影响评价[J].山地学报,2017,(04):437.[doi:10.16089/j.cnki.1008-2786.000240]
 LUO Yongzhong,GUO Xiaoqin,LIU Xuzhen.Impact of Climate Change on Grassland Productivity of Qilian Mountains in 1961-2013[J].Mountain Research,2017,(06):437.[doi:10.16089/j.cnki.1008-2786.000240]
[8]付建新,曹广超*,李玲琴,等.1960-2014年祁连山日照时数时空变化特征[J].山地学报,2018,(05):709.[doi:10.16089/j.cnki.1008-2786.000367]
 FU Jianxin,CAO Guangchao *,LI Lingqin,et al.Temporal and Spatial Variation Characteristics of Sunlight Hours in the Qilian Mountain,China from 1960 to 2014[J].Mountain Research,2018,(06):709.[doi:10.16089/j.cnki.1008-2786.000367]

备注/Memo

备注/Memo:
收稿日期(Received date):2014-10-11; 改回日期(Accepted): 2015-03-12。 作者简介(Biography):赵军(1963-),男,山西河津人,教授,博士生导师,主要从事资源环境遥感与GIS应用研究。[Zhao Jun(1963-), professor, doctoral supervisor, engaged in environmental remote sensing and GIS applied research.] E-mail:zhaojun@nwnu.edu.cn
更新日期/Last Update: 1900-01-01