[1] 肖生春,肖洪浪.黑河流域水环境演变及其驱动机制研究进展[J].地球科学进展,2008,23(7):748-755. [2] Cheng G D,Li X,Zhao W Z,et al.Integrated study of the water-ecosystem-economy in the Heihe River Basin[J].National Science Review,2014,1:413-428. [3] 司建华,冯起,张小由,等.黑河下游分水后的植被变化初步研究[J].西北植物学报,2005,25(4):631-640. [4] Su Y H,Feng Q,Zhu G F,et al.Identification and evolution of groundwater chemistry in the Ejin Sub-Basin of the Heihe River,Northwest China[J].Pedosphere,2007,17(3):331-342. [5] Xi H Y,Feng Q,Si J H,et al.Impacts of river recharge on groundwater level and hydrochemistry in the lower reaches of Heihe River Watershed,northwestern China[J].Hydrogeology Journal,2010,18:791-801. [6] Zhao W Z,Chang X L,He Z B.Responses of distribution pattern of desert riparian forests to hydrologic process in Ejina oasis[J].Science in China:Earth Sciences,2004,47(1):21-31. [7] 高冠龙,张小由,鱼腾飞,等.1987-2008年额济纳绿洲土地覆被变化及其驱动机制[J].中国沙漠,2015,35(3):821-829. [8] 廖杰,王涛,薛娴.黑河调水以来额济纳盆地湖泊蒸发量[J].中国沙漠,2015,35(1):228-232. [9] 肖生春.近2000 a黑河下游水环境演变及其驱动机制研究[D].北京:中国科学院研究生院,2006. [10] 额济纳旗志编纂委员会.额济纳旗志[M].北京:方志出版社,1998. [11] Mann M E,Bradley R S,Hughes M K.Global-scale temperature patterns and climate forcing over the past six centuries[J].Nature,1998,392(6678):779-787. [12] Speer J H.Frontiers in Dendrochronology[M]//Speer J H.Fundamentals of Tree-ring Research.Tucson,USA:The University of Arizona Press.2010:252-253. [13] Briffa K R.Annual climate variability in the Holocene:interpreting the message of ancient trees[J].Quaternary Science Reviews,2000,19:87-105. [14] Gou X H,Chen F H,Jacoby G,et al.Rapid tree growth with respect to the last 400 years in response to climate warming,northeastern Tibetan Plateau[J].International Journal of Climatology,2007,27(11):1497-1503. [15] Shao X M,Xu Y,Yin Z Y,et al.Climatic implications of a 3585-year tree-ring width chronology from the northeastern Qinghai-Tibetan Plateau[J].Quaternary Science Reviews,2010,29(17):2111-2122. [16] Yang B,Qin C,Wang J,et al.A 3,500-year tree-ring record of annual precipitation on the northeastern Tibetan Plateau[J].Proceedings of the National Academy of Sciences of the United States of America,2014,111(8):2903-2908. [17] Zhang Q B,Evans M N,Lyu L.Moisture dipole over the Tibetan Plateau during the past five and a half centuries[J].Nature Communications,2015,6:8062. [18] Schweingruber F H.Tree Rings and Environment:Dendroecology[M].Berne,Germany:Paul Haupt Publishers,1996. [19] Liang E Y,Shao X M,Eckstein D,et al.Spatial variability of tree growth along a latitudinal transect in the Qilian Mountains,northeastern Tibetan Plateau[J].Canadian Journal of Forest Research,2010,40(2):200-211. [20] Ren P,Rossi S,Gricar J,et al.Is precipitation a trigger for the onset of xylogenesis in Juniperus przewalskii on the north-eastern Tibetan Plateau?[J].Annals of Botany,2015,115(4):629-639. [21] Woodhouse C A.Extending hydrologic records with tree rings[J].Water Resources Impact,2000,2(4):25-27. [22] Gou X H,Deng Y,Chen F H,et al.Tree ring based streamflow reconstruction for the Upper Yellow River over the past 1234 years[J].Chinese Science Bulletin,2010,55(36):4179-4186. [23] Liu X H,Zhao L J,Chen T,et al.Combined tree-ring width and δ 13C to reconstruct snowpack depth:a pilot study in the Gongga Mountain,west China[J].Theoretical and Applied Climatology,2011,103(1):133-144. [24] Xiao S C,Xiao H L,Si J H,et al.Lake level changes recorded by tree rings of lakeshore shrubs:a case study at the Lake West Juyan,Inner Mongolia,China[J].Journal of Integrative Plant Biology,2005,47(11):1303-1314. [25] Xiao S C,Xiao H L,Dong Z B,et al.Dry/wet variation recorded by shrub tree-rings in the central Badain Jaran Desert of northwestern China[J].Journal of Arid Environments,2012,87:85-94. [26] Stoffel M,Bollschweiler M,Butler D R,et al.Tree Rings and Natural Hazards:A State-of-the-art[M].Dordrecht,Netherland:Springer,2010:1-502. [27] 刘恕.胡杨径向生长量对流域环境变化的指示意义[J].环境科学,1982,3(4):66-69. [28] Xiao S C,Xiao H L,Zhou M X,et al.Water level change of the West Juyan Lake in the past 100 years recorded in the tree ring of the shrubs in the lake banks[J].Journal of Glaciology and Geocryology,2004,26(5):557-562. [29] Xiao S C,Xiao H L,Peng X M,et al.Intra-annual stem diameter growth of Tamarix ramosissima and association with hydroclimatic factors in the lower reaches of China's Heihe River[J].Journal of Arid Land,2014,6(4):498-510. [30] Xiao S C,Xiao H L,Peng X M,et al.Hydroclimate-driven changes in the landscape structure of the terminal lakes and wetlands of the China's Heihe River Basin[J].Environmental Monitoring and Assessment,2015,187(1):1-14. [31] Xiao S C,Peng X M,Tian Q Y.Climatic and human drivers of recent lake-level change in East Juyan Lake,China[J].Regional Environmental Change,2015:1-11. [32] 刘普幸,陈发虎,勾晓华,等.额济纳旗近100 a来胡杨年表的建立与响应分析[J].中国沙漠,2005,25(5):764-768. [33] 孙军艳,刘禹,蔡秋芳.额济纳233年来胡杨树轮年表的建立及其所记录的气象水文变化[J].第四纪研究,2006,26(5):799-807. [34] 刘普幸,陈发虎,靳立亚,等.基于胡杨年轮重建黑河下游近100年春季径流量[J].干旱区地理,2007,30(5):696-700. [35] Zhang Q B,Li Z S,Liu P X,et al.On the vulnerability of oasis forest to changing environmental conditions:perspectives from tree rings[J].Landscape Ecology,2012,27:343-353. [36] 肖生春,肖洪浪,彭小梅.黑河下游胡杨季节尺度径向生长变化研究[J].冰川冻土,2012,34(3):706-712. [37] Peng X M,Xiao S C,Xiao H L.Preliminary dendrochronological studies on Populus euphratica in the lower reaches of the Heihe River basin in northwest China[J].Dendrochronologia,2013,31(3):242-249. [38] Peng X M,Xiao S C,Cheng G D,et al.Human activity impacts on the stem radial growth of Populus euphratica riparian forests in China's Ejina Oasis,using tree-ring analysis[J].Trees,2015.DOI:10.1007/s00468-00015-01287-z. [39] Liu X H,Wang W Z,Xu G B,et al.Tree growth and intrinsic water-use efficiency of inland riparian forests in northwestern China:evaluation via δ13C and δ18O analysis of tree rings[J].Tree Physiology,2014,34:966-980. [40] 程国栋.黑河流域水-生态-经济系统综合管理研究[M].北京:科学出版社,2009. [41] Su Y H,Zhu G,Feng Q,et al.Environmental isotopic and hydrochemical study of groundwater in the Ejina Basin,northwest China[J].Environmental Geology,2009,58(3):601-614. [42] Wang P,Yu J J,Zhang Y C,et al.Groundwater recharge and hydrogeochemical evolution in the Ejina Basin,northwest China[J].Journal of Hydrology,2013,476:72-86. [43] Zhu G F,Su Y H,Feng Q.The hydrochemical characteristics and evolution of groundwater and surface water in the Heihe River Basin,northwest China[J].Hydrogeology Journal,2007,16(1):167-182. [44] Grissino-Mayer H D.Evaluating crossdating accuracy:a manual and tutorial for the computer program COFECHA[J].Tree Ring Bulletin,2001,57:205-221. [45] Cook E R,Krusic P J.ARSTAN Version 41d:A Tree-ring Standardization Program Based on Detrending and Autoregressive Time Series Modeling,with Interactive Graphics[R].New York,USA:Tree-Ring Laboratory,Lamont Doherty Earth Observatory of Columbia University Palisades,2007. [46] Wigley T M L,Briffa K R,Jones P D.On the average value of correlated time series,with applications in dendroclimatology and hydrometeorology[J].Journal of Climate and Applied Meteorology,1984,23(2):201-213. [47] Briffa K R,Jones P D.Basic chronology statistics and assessment[M]//Cook E R,Kairiukstis L A.Methods of Dendrochronology:Applications in the Environmental Sciences.Dordrecht,Nertherland:Kluwer Academic Publishers,1990:137-152. [48] Briffa K R.Interpreting high-resolution proxy climate data-the example of dendroclimatology[M]//Von Storch H,Navarra A.Analysis of Climate Variability:Applications of Statistical Techniques.Berlin,Germany:Springer,1995:77-94. [49] Rodionov S N.A sequential algorithm for testing climate regime shifts[J].Geophysical Research Letters,2004,31(9):L09204. [50] Rodionov S N,Overland J E.Application of a sequential regime shift detection method to the Bering Sea ecosystem[J].ICES Journal of Marine Science:Journal du Conseil,2005,62(3):328-332. [51] Jin X M,Hu G C,Li W M.Hysteresis effect of runoff of the Heihe River on vegetation cover in the Ejina Oasis in Northwestern China[J].Earth Science Frontiers,2008,15(4):198-203. [52] Si J H,Feng Q,Cao S K,et al.Water use sources of desert riparian Populus euphratica forests[J].Environmental Monitoring and Assessment,2014,186(9):5469-5477. [53] 赵良菊,肖洪浪,程国栋,等.黑河下游河岸林植物水分来源初步研究[J].地理学报,2008,29(6):709-718. [54] 尹力,赵良菊,阮云峰,等.黑河下游典型生态系统水分补给源及优势植物水分来源研究[J].冰川冻土,2012,34(6):1478-1486. [55] Xi H Y.Study on the groundwater dynamics variation and numerical simulation in Ejina Basin[D].Beijing,China:University of the Chinese Academy of Sciences,2009. [56] 李小琴.荒漠河岸胡杨液流与叶水势特性研究[D].北京:中国科学院大学,2014. [57] 李炜.荒漠河岸胡杨林蒸腾耗水尺度扩展研究[D].北京:中国科学院大学,2013. [58] 石亮.明清及民国时期黑河流域中游地区绿洲化荒漠化时空过程研究[D].兰州:兰州大学,2010. [59] Liang E Y,Liu X H,Yuan Y J,et al.The 1920s drought recorded by tree rings and historical documents in the semi-arid and arid areas of Northern China[J].Climatic Change,2006,79(3/4):403-432. [60] Kang S Y,Yang B,Qin C,et al.Extreme drought events in the years 1877-1878,and 1928,in the southeast Qilian Mountains and the airesea coupling system[J].Quaternary International,2013,283:85-92. [61] Sun J Y,Liu Y.Drought variations in the middle Qilian Mountains,northeast Tibetan Plateau,over the last 450 years as reconstructed from tree rings[J].Dendrochronologia,2013,31(4):279-285. [62] 席海洋,冯起,司建华,等.黑河下游绿洲NDVI对地下水位变化的响应研究[J].中国沙漠,2013,33(2):574-582. |