Spacetime evolution for mid21st century water resources over the BeijingHangzhou Grand Canal under the IPCC_A1B scenario

XIA Hai-Bin; LE Qun; 

doi:10.3969/j.issn.1000-5641.2015.06.022

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Dec. 2015

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XIA Hai-Bin, LE Qun, . Spacetime evolution for mid21st century water resources over the BeijingHangzhou Grand Canal under the IPCC_A1B scenario[J]. Journal of East China Normal University (Natural Sciences), 2015, (6): 179-189. doi: 10.3969/j.issn.1000-5641.2015.06.022

Citation:

XIA Hai-Bin, LE Qun, . Spacetime evolution for mid21st century water resources over the BeijingHangzhou Grand Canal under the IPCC_A1B scenario[J]. Journal of East China Normal University (Natural Sciences), 2015, (6): 179-189. doi: 10.3969/j.issn.1000-5641.2015.06.022

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Spacetime evolution for mid21st century water resources over the BeijingHangzhou Grand Canal under the IPCC_A1B scenario

doi: 10.3969/j.issn.1000-5641.2015.06.022

XIA Hai-Bin^{1,2
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LE Qun²,


Received Date: 2014-12-11
Publish Date: 2015-11-25

Abstract

Abstract

With the successful application for the list of the World Heritage, the renaissance and activation of the BeijingHangzhou Grand Canal has become a focus, of which, the key is utilization and distribution of water resources of watershed along the Grand Canal. This article adopts the A1B scenario of IPCC in order to simulate space and time distribution of precipitation as well as its evolution characteristics both in Chinese modern times (later 20th century, represented by 1981-2000 twenty years annual mean value) and future times (middle 21th century, represented by 2041-2060 twenty years annual mean value). This scenario simulation aims to analyze the spacetimechange characteristics of water resources of the Grand Canal. It reveals that from north to south, the volume of water resources of the Yangtze River Valley will decrease, while that of Huaihe River Valley will increase significantly. And that of the Huanghe River Valley and the Haihe River Valley will rise up slightly. Therefore, it concludes that the key of navigationof the GrandCanal is to use as early as possible the water resources of the Huaihe River Valley to transfer water resources in the south valley of Huanghe River to the north valley, and achieve navigation of the Grand Canal in the north of Huanghe Valley as well as to restore the diversion works in Nanwang and Northern five Lakes Reservoir in the context of SouthtoNorth Water Diversion Project so that the GrandCanal world heritage could be preserved. 
- BeijingHangzhou Grand CanalIPCC_A1B Scenarioglobal changeprecipitation variation,

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References

[1]

［1］俞孔坚, 李迪华, 李伟. 论大运河区域生态基础设施战略和实施途径［J］. 地理科学进展, 2004, 23(1): 112.

［2］张志兵, 施心路, 杨仙玉, 等. 杭州西湖与京杭大运河杭州城区段水质对比研究［J］. 杭州师范大学学报: 自然科学版, 2011, 10(1): 5963.

［3］毛锋, 王凌云, 周文生,等. 大运河历史文化环境保护支持系统［J］. 清华大学学报：自然科学版, 2007, 47(9):14011404.

［4］黄震方, 李芸, 王勋. 京杭大运河旅游产品体系的构建及其旅游开发——以京杭大运河江苏段为例［J］. 地域研究与开发, 2000, 19(1)：7072.

［5］李书恒, 郭伟. 京杭大运河的功能与苏北运河段的发展利用［J］. 第四纪研究, 2007, 27(5):861869.

［6］谭徐明, 于冰, 王英华,等. 京杭大运河遗产的特性与核心构成［J］. 水利学报, 2009, 40(10):12191226.

［7］方修泮, 郝玉明, 孙晋明. 结合南水北调东线工程实现京杭运河（济宁天津段）复航［J］.水运工程, 2005, (12):5054.

［8］GRAY V. Climate change 2007: The physical science basis summary for policymakers［J］. Energy & Environment, 2007, 18(3): 433440.

［9］GOLODETS C, STERNBERG M, KIGEL J, et al. From desert to Mediterranean rangelands: Will increasing drought and interannual rainfall variability affect herbaceous annual primary productivity?［J］. Climatic Change, 2013, 119(34):785798.

［10］姚汉源. 京杭运河史［M］.北京: 中国水利水电出版社, 1998：35.

［11］陈诗越, 吴金甲. 运河水柜——南四湖与北五湖的历史与变迁［J］. 聊城大学学报: 社会科学版, 2014 (4): 1519.

［12］刘建刚, 邓俊, 谭徐明, 等. 京杭运河全线复航的水资源条件论证［C］// 2013 年中国水利学会水利史研究会学术年会暨中国大运河水利遗产保护与利用战略论坛论文集, 2013.

［13］杨登琴. 京杭运河与南水北调东线的关系［J］. 治淮, 1997, 12（5）: 2830.

［14］方修泮, 郝玉明, 孙晋明. 结合南水北调东线工程实现京杭运河（济宁天津段）复航［J］. 水运工程, 2005, (12):5054.

［15］GIORGI F, PAL J S, BI X, et al. Introduction to the TAC special issue: The RegCNET network［J］. Theoretical and Applied Climatology, 2006, 86(14): 14.

［16］GIORGI F, MEARNS L O. Introduction to special section: Regional climate modeling revisited［J］. Journal of Geophysical Research: Atmospheres (1984-2012), 1999, 104(D6): 63356352.

［17］刘绿柳, 姜彤, 原峰. 珠江流域1961-2007年气候变化及2011-2060年预估分析［J］. 气候变化研究进展, 2009, 5(4):209214.

［18］邓慧平, 吴正方, 唐来华. 气候变化对水文和水资源影响研究综述［J］. 地理学报, 1996, 51:161170.

［19］BUYTAERT W, CéLLERI R, TIMBE L. Predicting climate change impacts on water resources in the tropical Andes: Effects of GCM uncertainty［J］. Geophysical Research Letters, 2009, 36(7):157163.

［20］江志红, 张霞, 王冀. IPCCAR4模式对中国21世纪气候变化的情景预估［J］. 地理研究, 2008, 27(4):787799.

［21］胡伯彦, 汤剑平, 王淑瑜. 中国地区IPCC A1B情景下21世纪中期气候变化的数值模拟试验［J］. 气象科学, 2012, 32(2):127136.

［22］钟军, 苏布达, 翟建青,等. 中国日降水的分布特征和未来变化［J］. 气候变化研究进展, 2013, 9(2):8995.

［23］郝振纯, 鞠琴, 王璐,等. 气候变化下淮河流域极端洪水情景预估［J］. 水科学进展, 2011, 22(5):605614.

［24］刘恒, 耿雷华, 陈晓燕. 区域水资源可持续利用评价指标体系的建立［J］. 科技传播, 2003, (3):265270.

［25］张永勤, 缪启龙, 何毓意,等. 区域水资源量的估算及预测分析——以南京地区为例［J］. 地理科学, 2001, 21(5):457462.

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