全部 标题 作者
关键词 摘要

OALib Journal期刊
ISSN: 2333-9721
费用:99美元

查看量下载量

相关文章

更多...

青藏高原50年来水循环要素变化趋势及其区域差异性

Keywords: 水文环境,青藏高原,降水

Full-Text   Cite this paper   Add to My Lib

Abstract:

基于气象台站、再分析资料分析以及过去研究成果的综合,系统总结了过去50年青藏高原水文环境变化趋势及其区域差异性。显著、同步的地表升温是青藏高原水分循环最为显著驱动特征。日照、风速的下降形成大气驱动因子的减弱,表现为蒸发力下降。大气水汽含量与其他因子造成降水量微弱增加,但区域差异明显。随着地表气温上升,最大积雪水当量减少、冻土活动层厚度增加。尽管蒸发力下降,地表土壤湿度的增加依然导致蒸散发微弱增加。

References

[1]  姚檀栎,朱立平.青藏高原环境变化对全球变化的响应及其适应对策.地球科学进展,2006, 21 (5):459~464
[2]  Yao Tandong, Zhu Liping.The response of environmental changes on Tibetan Plateau to global changes and adaptation strategy.Advances in Earth Science,2006, 21 (5):459~464
[3]  IPCC. Climate Change 2007: The Physical Science Basis.Cambridge: Cambridge University Press,2007.345~348
[4]  Liu X, Chen B. Climatic warming in the Tibetan Plateau during recent decades.International Journal Climatology,2000, 20 (14):1729~1742 3.0.CO;2-Y target="_blank">
[5]  曹建廷,秦大河,康尔泗等.青藏高原外流区主要河流的径流变化.科学通报,2005, 50 (21):2403~2408
[6]  Cao Jianting,Qin Dahe,Kang Ersi et al.River discharge changes in the Qinghai-Tibet Plateau.Chinese Science Bulletin,2005, 51 (5):594~600
[7]  Gao Zhiyou,Wang Xiaodan,Yin Guan.Hydrological rule and isotopic composition of water bodies in Yarlung Zangbo River.Acta Geographica Sinica,2007, 62 (9):1002~1007
[8]  安 全,梁 川,刘 政,雅砻江中上游径流变化特性的小波分析.武汉大学学报(工学版),2008, 41 (3): 20~28
[9]  An Quan,Liang Chuan,Liu Zheng.Wavelet analysis of runoff variation characteristics in upper-middle reaches of Yalong River.Engineering Journal of Wuhan University,2008, 41 (3):20~28
[10]  马晓波,胡泽勇.青藏高原40 年来降水变化趋势及突变的分析.中国沙漠,2005, 25 (1):137~139
[11]  Ma Xiaobo,Hu Zeyong.Precipitation variation characteristics and abrupt change over Qinhai-Xizang Plateau in recent 40 years.Journal of Desert Research,2005, 25 (1):137~139
[12]  张 磊,缪启龙.青藏高原近40年来的降水变化特征.干旱区地理,2007, 30 (2):240~246
[13]  Zhang Lei,Miao Qilong.Precipitation changes in the Tibetan Plateau during the last four decades.Arid Land Geography,2007, 30 (2):240~246
[14]  段克勤,姚檀栋,王宁练等.青藏高原南北降水变化差异研究.冰川冻土,2008, 30 (5):726~732
[15]  Duan Keqin,Yao Tandong,Wang Ninglian et al.The difference in precipitation variability between the North and South Tibetan Plateaus.Journal of Glaciology and Geocryology,2008, 30 (5):726~732
[16]  Stanhill G, Cohen S.Global dimming: A review of the evidence for a widespread and significant reduction in global radiation.Agriculture and Forest Meteorology,2001, 107,255~278,doi: 10.1016/S0168-1923(00)00241-0
[17]  Zhang Y, Liu C,Tang Y et al.Trends in pan evaporation and reference and actual evapotranspiration across the Tibetan Plateau.Journal of Geophysical Research,2007, 112,D12110,doi: 10.1029/2006JD008161
[18]  Zhang X, Ren Y,Yin Z-Y et al.Spatial and temporal variation patterns of reference evapotranspiration across the Qinghai-Tibetan Plateau during 1971~2004.Journal of Geophysical Research,2009, 114,D15105,doi: 10.1029/2009JD011753
[19]  高 荣,韦志刚,董文杰等.20 世纪后期青藏高原积雪和冻土变化及其与气候变化的关系.高原气象,2003, 22 (2):191~196
[20]  Gao Rong,Wei Zhigang,Dong Wenjie et al.Variation of the snow and frozen soil over Qinghai-Xizang Plateau in the late twentieth century and their relations to climatic change.Plateau Meteorology,2003, 22 (2):191~196
[21]  Osterkamp T E. Characteristics of the recent warming of permafrost in Alaska.Journal of Geophysical Research,2007, 112, F02S02,doi:10.1029/2006JF000578
[22]  Pavlov A V. Permafrost-climate monitoring of Russia: Analysis of field data and forecast.Polar Geography, 1996, 20 (1):44~64
[23]  Wu Q B, Zhang T J.Recent permafrost warming on the Qinghai-Tibetan Plateau.Journal of Geophysical Research, 2008, 113, D13108,doi:10.1029/2007JD009539
[24]  Sharkhuu N. Recent changes in the permafrost of Mongolia.In: Phillips M,Springman S M,Arenson L U eds.Proceedings of the 8th International Conference on Permafrost,21~25 July 2003,Zurich,Switzerland.A.A.Balkema,Lisse,the Netherlands,2003.1029~1034
[25]  Harris C, Mühll D V,Isaksen K et al.Warming permafrost in European mountains.Global Planet Change,2003, 39 (3):215~225
[26]  Allison I, Barry R G,Goodison B E.Climate and Cryosphere(CliC)Project Science and Co-ordination Plan.WCRP-114/WMO/TD,No.1053,2001
[27]  程国栋.冰冻圈变化研究专辑序言.冰川冻土,1996, 18 (增刊):1~3
[28]  Cheng Guodong.Preface for special issue of cryospheric changes.Journal of Glaciology and Geocryology,1996, 18 (S1):1~3
[29]  王绍令.青藏高原冻土退化的研究.地球科学进展,1997, 12 (2):164~167
[30]  Wang Shaoling.Study on permafrost retreat in Tibetan Plateau.Advances in Earth Science,1997, 12 (2):164~167
[31]  Anisimov O A, Shiklomanov N I,Nelson F E.Global warming and active-layer thickness: Results from transient general circulation models.Global Planet Change,1997, 15 (3~4):61~78
[32]  裴超重,钱开铸,吕京京等.长江源区蒸散量变化规律及其影响因素.现代地质,2010, 24 (2):362~368
[33]  Pei Chaozhong,Qian Kaizhu,Lü Jingjing et al.The variation of evapotraspiration and the impacts on it in the source region of the Yangtze River.Geoscience,2010, 24 (2); 362~368
[34]  谢昌卫,丁永建,刘时银等.长江、黄河源寒区径流时空变化特征对比.冰川冻土,2003, 25 (4):415~422
[35]  Xie Changwei,Ding Yongjian,Liu Shiyin et al.Comparison analysis of runoff change in the source regions of the Yangtze and Yellow Rivers.Journal of Glaciology and Geocryology,2003, 25 (4):415~422
[36]  高 冰,杨大文,刘志雨等.雅鲁藏布江流域的分布式水文模拟及径流变化分析.水文,2008, 28 (3):40~44
[37]  Gao Bing,Yang Dawen,Liu Zhiyu et al.Application of a distributed hydrological model for the Yarlung Zangbo River and analysis of the river runoff.Journal of China Hydrology,2008, 28 (3):40~44
[38]  高志友,王小丹,尹 观.雅鲁藏布江径流水文规律及水体同位素组成.地理学报,2007, 62 (9):1002~1007

Full-Text

Contact Us

service@oalib.com

QQ:3279437679

WhatsApp +8615387084133