[1] Baker V R. Palaeoflood hydrology in a global context. Catena, 2006, 66(1/2): 161-168. [2] Nathan A Sheffer, Mayte Rico, Yehouda Enzel et al. The palaeoflood record of the Gardon River, France: A comparison with the extreme 2002 flood event. Geomorphology, 2008, 98: 71-83. [3] Huang Chunchang, Pang Jiangli, Zha Xiaochun et al. Extraordinary hydro-climatic events during the period AD 200-300 recorded by slackwater deposits in the upper Hanjiang River valley, China. Palaeogeography, Palaeoclimatology, Palaeoecology, 2013, 374: 274-283. [4] Knox J C. Sensitivity of modern and Holocene floods to climate change. Quaternary Science Reviews, 2000, 19: 439-457. [5] Benito G, Thorndycraft V R, Rico M et al. Palaeo flood and floodplain records from Spain: Evidence for long-term climate variability and environmental changes. Geomorphology, 2008, 101: 68-77. [6] Kochel R C, Baker V R. Palaeoflood hydrology. Science, 1982, 215: 353-361. [7] Zhan Daojiang, Xie Yuebo. Palaeoflood Study. Beijing: China WaterPower Press, 2001: 1-83.[詹道江, 谢悦波. 古洪水 研究. 北京: 中国水利水电出版社, 2001: 1-83.] [8] Alpa S. A mid-late Holocene flood record from the alluvial reach of the Mahi River, western India. Catena, 2007, 70: 330-339. [9] Gerardo B, Alfonso S, Yolanda S et al. Palaeoflood record of the Tagus River (Central Spain) during the Late Pleistocene and Holocene. Quaternary Science Reviews, 2003, 22: 1737-1756. [10] Yael Jacoby, Tamir Grodek, Yehouda Enzel. Late Holocene upper bounds of flood magnitudes and twentieth century large floods in the ungauged, hyperarid alluvial Nahal Arava, Israel. Geomorphology, 2008, 95: 274-294. [11] Ortega J A, Garz′on G. A contribution to improved flood magnitude estimation in base of palaeoflood record and climatic implications. Natural Hazards and Earth System Sciences, 2009, 9: 229-239. [12] England J F Jr, Godaire J E, Klinger R E et al. Paleohydrologic bounds and extreme flood frequency of the upper Arkansas River, Colorado, USA. Geomorphology, 2010, 124: 1-16. [13] Webb R H, Jarrett R. D. One-dimensional estimation techniques for discharges of paleofloods and historical floods. Water Science and Application, 2002, 5: 111-125. [14] Yang Dayuan, Ge Yu, Xie Yuebo et al. Sedimentary records of large Holocene floods from the middle reaches of the Yellow River, China. Geomorphology, 2000, 33(1/2): 73-88. [15] Huang Chunchang, Pang Jiangli, Zha Xiaochun et al. Sedimentary records of the extraordinary floods at the ending of the mid-Holocene Climatic Optimum along the upper Weihe River, China. Holocene, 2012, 22(6), 675-686. [16] Huang Chunchang, Pang Jiangli, Zha Xiaochun. Holocene palaeoflood events recorded by slackwater deposits along the upper Jinghe River valley, middle Yellow River basin, China. Journal of Quaternary Science, 2012, 27(5), 485-493. [17] Huang Chunchang, Pang Jiangli, Zha Xiaochun et al. Extraordinary floods related to the climatic event at 4200 a BP on the Qishuihe River, middle reaches of the Yellow River, China. Quaternary Science Reviews, 2011, 30: 460-468. [18] Huang Chunchang, Pang Jiangli, Zha Xiaochun et al. Extraordinary floods of 4100-4000 a BP recorded at the Late Neolithic ruins in the Jinghe River gorges, middle reach of the Yellow River, China. Palaeogeography, Palaeoclimatology, Palaeoecology, 2010, 289(3): 1-9. [19] Xie Yuebo, Fei Yuhong, Shen Qipeng. Slack water deposits and flow peak level of a paleoflood. Acta Geoscientia Sinica, 2001, 22(4): 320-323.[谢悦波, 费宇红, 沈起鹏. 古洪水平流沉积与水位. 地球学报, 2001, 22(4): 320-323.] [20] Huang Chunchang, Li Xiaogang, Pang Jiangli et al. Palaeoflood sedimentological and hydrological studies on the Yongheguan reach in the middle Yellow River. Acta Geographica Sinica, 2012, 67(11): 1493-1504.[黄春长, 李晓刚, 庞奖励等. 黄河永和关段全新世古洪水研究. 地理学报, 2012, 67(11): 1493-1504.] [21] Shi Fucheng, Yi Yuanjun, Mu Ping. Investigation, Research and Study on the Yellow River Historical Flood. Zhengzhou: Yellow River Water Conservancy Press, 2002: 81-123.[史辅成, 易元俊, 慕平. 黄河历史洪水调查、考证 和研究. 郑州: 黄河水利出版社, 2002: 81-123.] [22] Li Wenhao. Hydrologic characteristics analysis in the upper reaches of Hanjiang River. Journal of Water Resources & Water Engineering, 2004, 15(2): 54-58.[李文浩. 汉江上游流域水文特性分析. 水资源与水工程学报, 2004, 15(2): 54-58.] [23] Zhang Kai. Analyses of rainstorm and flood characteristics in the upper reaches of Hanjiang River. Journal of Catastrophology, 2006, 21(3): 98-102.[张楷. 汉江上游暴雨洪水特性研究. 灾害学, 2006, 21(3): 98-102.] [24] He Sudi. Characteristics of soil erosion in Hanjiang valley and possble countermeasures. Resources and Environment in the Yangtze Basin, 1997, 6(3): 271-276.[贺素娣. 汉江流域水土流失特点及防治对策. 长江流域资源与环境, 1997, 6(3): 271-276.] [25] Yang Yongde, Zou Ning, Guo Xiwang et al. Analysis and calculation of design flood at Baihe gauge station in Hanjiang River. Water Resources Research, 1997, 18(3): 36-38.[杨永德, 邹宁, 郭希望等. 汉江白河水文站设计洪水 分析计算. 水资源研究, 1997, 18(3): 36-38.] [26] Huang Chunchang, Pang Jiangli, Zha Xiaochun et al. Prehistorical floods in the Guanzhong Basin in the Yellow River drainage area: A case study along the Qishuihe River Valley over the Zhouyuan Loess Tableland. Sci. Sin. Terrae, 2011, 41: 1658-1669.[黄春长, 庞奖励, 查小春等. 黄河流域关中盆地史前大洪水研究: 以周原漆水河谷地为例. 中 国科学, 2011, 41: 1658-1669.] [27] Zha Xiaochun, Huang Chunchang, Pang Jiangli et al. The Holocene palaeoflood events in the Yunxi Reach in the upper reaches of Hanjiang River. Acta Geographica Sinica, 2012, 67(5): 671-680.[查小春, 黄春长, 庞奖励等. 汉江上 游郧西段全新世古洪水事件研究. 地理学报, 2012, 67(5): 671-680.] [28] Li Xiaogang, Huang Chunchang, Pang Jiangli et al. Palaeoflood hydrological study in the Baihe Reach in the upper reaches of the Hanjiang River. Scientia Gepgraphica Sinica, 2012, 32(8): 971-978.[李晓刚, 黄春长, 庞奖励等, 汉江 上游白河段万年尺度洪水水文学研究. 地理科学, 2012, 32(8): 971-978.] [29] Xu Jie, Huang Chunchang, Pang Jiangli et al. Sedimentological and hydrological studies of the palaeoflood events in the Ankang east section in the upper reaches of the Hanjiang River. Journal of Lake Sciences, 2013, 25(3): 445-454.[许洁, 黄春长, 庞奖励等. 汉江上游安康东段全新世古洪水沉积学与水文学研究. 湖泊科学, 2013, 25(3): 445-454.] [30] Zhang Yuzhu., Huang Chunchang, Pang Jiangli et al. Holocene palaeofloods related to climatic events in the upper reaches of the Hanjiang River valley, middle Yangtze River Basin, China. Geomorphology, 2013, 195: 1-12. [31] Qin Jiaming, Yuan Daoxian, Cheng Hai et al. The Y. D. and climate abrupt events in the early and middle Holocene:stalagmite oxygen isotope record from Maolan, Guizhou, China. Science in China: Series D, 2005, 48(4): 530-537. [32] Gasse, F. Diatom-inferred salinity and carbonate oxygen isotopes in Holocene waterbodies of the western Sahara and Sahel (Africa). Quaternary Science Reviews, 2002, 21: 737-767. [33] Mayewski P A, Meeker L D. Major features and forcing of high-latitude northern hemisphere atmospheric circulation using a 110, 000-year long glaciochemical series. Journal of Geophysical Research, 1997, 102: 26345-26366. [34] Meese D A, Gow A J, Grootes P et al. The accumulation record from the GISP2 Core as an indicator of climate change throughout the Holocene. Science 1994, 266: 1680-1682. [35] US Army Corps of Engineers HEC. HEC-RAS River Analysis System Hydraulic Reference Manual. Davis, California, USA, 2010. [36] School of Water Resource and Hydropower. Hydraulics. Beijing: Higher Education Press, 1986: 335-336.[武汉水利电 力学院水力学教研室. 水力学. 北京: 高等教育出版社, 1986: 335-336.] [37] Chow V T. Open-channel Hydraulics. New York: McGraw-Hill Book Company Inc., 1959. [38] O'Connor J E, Webb R H. Hydraulic modelling for paleoflood analysis//Baker V R, Kochel R C, Patton P C. Flood Geomorphology. New York: Wiley, 1988: 393-402. |