气候变化对青藏高原高寒草甸适宜气候分布范围的潜在影响

doi:10.11733/j.issn.1007-0435.2009.06.002

›› 2009, Vol. 17 ›› Issue (6): 699-705.DOI: 10.11733/j.issn.1007-0435.2009.06.002

气候变化对青藏高原高寒草甸适宜气候分布范围的潜在影响

吴建国, 吕佳佳

中国环境科学研究院, 北京, 100012

收稿日期:2009-05-18 修回日期:2009-07-06 出版日期:2009-12-15 发布日期:2009-12-15
作者简介:吴建国(1971- ),男,博士,副研究员,主要从事气候变化的影响与适应,E-mail:wujg9298@yahoo.com.cn
基金资助:
国家“十一五”科技支撑项目(2007BAC03A02-06);中国环境科学研究院公益性院所基金项目(2007KYYW05)支持

The Potential Impact of Climate Change on the Suitable Climatic Distribution Region of Alpine Meadows in Qinghai-Tibet Plateau

WU Jian-guo, Lü Jia-jia

Chinese Research Academy of Environmental Sciences, Beijing 100012, China

Received:2009-05-18 Revised:2009-07-06 Online:2009-12-15 Published:2009-12-15

摘要/Abstract

摘要： 为确定气候变化对高寒草甸分布范围的影响,以Holdridge生命地带性分类系统,采用A1、A2、B1、B2气候变化情景,分析了气候变化对我国高寒草甸潜在适宜气候分布范围的影响.结果显示:气候变化下,高寒草甸基准情景下适宜气候分布范围将减少,新适宜气候分布范围将增加,总的适宜气候分布范围变化不大,其中A1、A2情景下变化较大,B1、B2气候情景下变化较小;高寒草甸在基准情景下适宜气候分布范围的最小、最大值与中位数都将减少,新适宜气候扩展范围的最小、最大值与中位数将增加,总的适宜气候分布范围的最小、最大值与中位数变化不大;高寒草甸基准情景下适宜气候分布区南部范围将缩小,新的适宜气候分布范围将主要朝西部和西北部方向扩展,其中A1情景下变化最大,B1情景下变化较小;高寒草甸基准情景下适宜气候分布范围和新的适宜气候分布范围与我国年均气温变化和年降水量变化呈现正相关性.从而预测,气候变化使高寒草甸在基准情景下的气候分布范围将减小,新的适宜分布范围将扩大,空间分布格局将发生改变.

关键词: 气候变化, 高寒草甸, 气候适宜范围

Abstract: It is crucial to understanding the effects of climate change on the distribution of terrestrial ecosystem for the environmental protection following climate change.The alpine meadow is an ecosystem type sensitive and vulnerable to climate change.To understand the impacts of climate change on the potential distribution of alpine meadows,the effects of climate change on the suitable climatic distribution region of alpine meadows in Qinghai-Tibet plateau were analyzed using Holdridge Life Zone System under climate change scenarios of A1,A2,B1 and B2.The results show that climate change in China would cause a decrease in the suitable climatic distribution region of alpine meadows under baseline climate scenario,an increase in the new suitable climatic distribution region of alpine meadows,while no change in total suitable climatic distribution region of alpine meadows.And climate change in China would also cause a decrease in the minimum,maximum,and median of suitable climatic distribution region of alpine meadows under baseline climate scenario,an increase in the minimum,maximum and median of new suitable climatic distribution region of alpine meadows,and no change in the minimum,maximum and median of total suitable climatic distribution region of alpine meadows.Additionally,following climate change,the south of suitable climatic distribution region of alpine meadows under baseline climate scenario would reduce,and new suitable climatic distribution region would expand mainly towards west and northwest of suitable climatic distribution region of alpine meadows under baseline climate scenario,and they were the highest in A1 scenario and the lowest in B1 scenario among climate change scenarios of A1,A2,B1 and B2 following climate change.Following climate change,the change of the suitable climatic distribution region under baseline climate scenario,new suitable climatic distribution region,and total suitable climatic distribution region of alpine meadows were all positively correlated with the changes in annual mean air temperature and precipitation in China,and the effects of increasing annual mean air temperature in China were higher than that of increasing annual precipitation.The results indicate that climate change in China would cause a decrease in the distribution region under baseline climate scenario and an increase in the expanding distribution region of alpine meadows,and the spatial distribution pattern would change greatly.

Key words: Climate change, Alpine meadows, Suitable climatic distribution region

中图分类号:

S162
S812.1

吴建国, 吕佳佳. 气候变化对青藏高原高寒草甸适宜气候分布范围的潜在影响[J]. , 2009, 17(6): 699-705.

WU Jian-guo, Lü Jia-jia. The Potential Impact of Climate Change on the Suitable Climatic Distribution Region of Alpine Meadows in Qinghai-Tibet Plateau[J]. , 2009, 17(6): 699-705.

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参考文献

[1] The Intergovernmental Panel of Climate Change(IPCC).Climate Change 2007.Impacts adaptations and vulnerability:fourth assessment report of working group II[R]. Cambridge,UK:Cambridge University Press,2007.232-272.
[2] 周兴明.中国嵩草草甸[M]. 北京:科学出版社,2001,1-23.
[3] 姚玉璧,张秀云,王润元,等.亚高山草甸华灰早熟禾对气候变化的响应[J]. 应用生态学报,2009,20(2):285-292.
[4] 赵茂盛,Neilson R P,延晓冬,等.气候变化对中国植被可能影响的模拟[J]. 地理学报,2002,57(1):28-38.
[5] Smith B,Prentice I C,Sykes M T.Representation of vegetation dynamics in the modeling of terrestrial ecosystem:comparing two contrasting approaches within European climate space[J]. Global Ecology And Biogeography,2001,10:621-637.
[6] Smith S J,Thomson A M,Rosenberg N J,et al.Climate change impacts for the conterminous USA:an integrated assessment.Part.scenarios and context[J]. Climate Change,2005,69:7-25.
[7] 张新时,杨奠安,倪文革.植被的PE(可能蒸散)指标与植被-气候分类(三)-几种主要方法与PEP程序介绍[J]. 植被生态学与地植物学学报,1993,17(2):97-109.
[8] Velardea S J,Malhib Y,Morand D T,et al.Valuing the impacts of climate change on protected areas in Africa[J]. Ecological Economics,2005,53,21-33.
[9] Chapin F S,Krner C.Arctic and alpine biodiversity:patterns,causes and ecosystem consequences[M]. Ecological studies113.Berlin,Germany:Springer-Verlag,1995.45-62.
[10] 吴征镒.中国植被(第二版)[M]. 北京:科学出版社,1995,642-657.
[11] 张家诚.中国气候总论[M]. 北京:气象出版社,1991.256-280.
[12] 中华人民共和国农业部畜牧兽医司,全国畜牧兽医总站.中国草地资源[R]. 北京:中国科学技术出版社,1996,1-366.
[13] 王绍武,董光荣.中国西部环境演变评估.第一卷.中国西部环境特征及其演变[M]. 北京:科学出版社,2002,29-70.
[14] 张新时.植被的PE(可能蒸散)指标与植被-气候分类(一)-几种主要方法与PEP程序介绍[J]. 植被生态学与地植物学学报,1989a,13(1):1-9.
[15] 张新时.植被的PE(可能蒸散)指标与植被-气候分类(二)-几种主要方法与PEP程序介绍[J]. 植被生态学与地植物学学报,1989b,13(3):197-207..
[16] 刘春迎.KIRA 指标在中国植被与气候关系中应用[J]. 植物生态学报,1999,23(2):125-138.
[17] Holdridge L R.Determination of world plant formations from simple climate data[J]. Science,1947,105(27):367-368.
[18] Yue T-X,Liu J-Y,Jrgensen S-E,et al.Changes of Holdridge life zone diversity in all of China over half a century[J]. Ecological Modeling,2001,144:153-162.
[19] Zheng Y,Xie Z,Jiang L,et al.Changes in Holdridge Life Zone diversity in the Xinjiang Uygur Autonomous Region(XUAR) of China over the past 40 years[J]. Journal of Arid Environments,2006,66:113-126.
[20] 周广胜,王玉辉.全球生态学[M]. 北京:气象出版社,2003,108-154.
[21] 许吟隆,黄莺翘,张勇,等.中国21世纪气候变化情景分析[J]. 气候变化进展,2005,1(2):80-83.
[22] 许吟隆,薛峰,林一骅.不同温室气体排放情景下中国21世纪地面气温和降水变化的模拟分析[J]. 气候与环境研究,2002,8(2):207-217.
[23] 许吟隆.中国21世纪气候变化的情景模拟分析[J]. 南京气象学院学报,2005,28(3):323-329.
[24] 居辉,熊伟,许吟隆,等.气候变化对我国小麦产量的影响[J]. 作物学报,2005,31(10):1340-1343.
[25] 熊伟,许吟隆,林而达,等.两种温室气体排放方案下我国水稻产量变化模拟[J]. .应用生态学报,2005,16(1):65-68.
[26] Houghton J T,Ding Y,Griggs G J,et al.IPCC climate change 2001,the scientific basis:contribution of working group one to the third assessment report of the intergovernmental panel of climate change[R]. Cambridge,UK:Cambridge University Press,2001.525-638.
[27] 张新时,刘春迎.全球变化条件下青藏高原植被变化图景预测[A]. 见:中国国家自然科学基金委员会生命科学部,中国科学院上海文献情报中心编.全球变化与生态系统[C]. 上海:上海科学技术出版社,1994.17-26.
[28] 吴建国,吕佳佳.气候变化对我国干旱区范围的潜在影响[J]. 环境科学研究,2009,22(2):199-206.
[29] Hitz S,Smith J.Estimating global impacts from climate change[J]. Global Environmental Change,2004,14:201-218.
[30] Leemans R,Eickhout B.Another reasons for concern:regional and global impacts on ecosystem for different levels of climate change[J]. Global Environmental Changes,2004,14:219-228.
[31] 姚德良,张强,沈振西,等.高寒草甸小气候考察研究[J]. 草地学报,2003,11(4):301-305.
[32] 王瑞永,刘莎莎,王成章,等.不同海拔高度高寒草地土壤理化指标分析[J]. 草地学报,2009,17(5):621-628

气候变化对青藏高原高寒草甸适宜气候分布范围的潜在影响

The Potential Impact of Climate Change on the Suitable Climatic Distribution Region of Alpine Meadows in Qinghai-Tibet Plateau

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