[1] 毛萍,黄东晓,王芋华,等.全球变化领域研究现状与趋势的大数据分析[J].中国科学院大学学报,2017,34(4):441-451.
[2] 陈泮勤.国际地圈、生物圈计划——全球变化的研究[J].中国科学院院刊,1987(3):206-211.
[3] 李克让,陈育峰.中国全球气候变化影响研究方法的进展[J].地理研究,1999,18(2):214-219.
[4] 李江风,袁玉江,由希尧.树木年轮水文学研究与应用[M].北京:科学出版社,2000.
[5] Rydval M,Gunnarson B E,Loader N J,et al.Spatial reconstruction of Scottish summer temperatures from tree rings[J].International Journal of Climatology,2017,37(3):1540-1556.
[6] Liu Y,An Z S,Linderholm H W.Annual temperatures during the last 2485 years in the mid-eastern Tibetan Plateau inferred from tree rings[J].Science in China Series D:Earth Sciences,2009,529(3):348-359.
[7] Tejedor E,Saz M A,Esper J,et al.Summer drought reconstruction in Northeastern Spain inferred from a tree-ring latewood network since 1734[J].Geophysical Research Letters,2017,44(16):8492-8500.
[8] Tejedor E,De L M,Cuadrat J M,et al.Tree-ring-based drought reconstruction in the Iberian Range(east of Spain) since 1694[J].International Journal of Biometeorology,2016,60(3):1-12.
[9] Gou X H,Gao L,Deng Y,et al.An 850-year tree-ring-based reconstruction of drought history in the western Qilian Mountains of northwestern China[J].International Journal of Climatology,2015,35(11):3308-3319.
[10] Shao X M,Huang L,Liu H.Reconstruction of precipitation variation from tree rings in recent 1000 years in Delingha,Qinghai[J].Science in China Ser.D Earth Sciences,2005,48(7):939-949.
[11] Li J B,Gou X H,Cook E R,et al.Tree-ring based drought reconstruction for the central Tien Shan area in northwest China[J].Geophysical Research Letters,2006,33(7):L07715.
[12] Chen F,Yuan Y J,Wei W S,et al.Precipitation reconstruction for the southern Altay Mountains(China) from tree rings of Siberian spruce,reveals recent wetting trend[J].Dendrochronologia,2014,32(3):266-272.
[13] Shi J,Lu H,Li J.Tree-ring based February-April precipitation reconstruction for the lower reaches of the Yangtze River,southeastern China[J].Global & Planetary Change,2015,131:82-88.
[14] Cai Q F,Yu L.Two centuries temperature variations over subtropical southeast China inferred from Pinustaiwanensis,Hayata tree-ring width[J].Climate Dynamics,2017,48(5/6):1813-1825.
[15] 杨婷婷,刘朋涛,刘同海,等.正蓝旗沙漠化草地分布格局及2002-2011年动态变化的遥感监测[J].干旱区资源与环境,2013,27(10):181-185.
[16] 白美兰,郝润全.气候变化对浑善达克沙地生态环境演变的影响[J].中国沙漠,2006,26(3):484-488.
[17] 刘树林,王涛.浑善达克沙地的土地沙漠化过程研究[J].中国沙漠,2007,27(5):719-724.
[18] 包斯琴,高科,王桂花.浑善达克沙地东部地区沙漠化发展近今演变研究——正蓝旗境内沙漠化研究为例[J].内蒙古农业大学学报(自然科学版),2006,27(2):25-29.
[19] 杨银科,黄强,刘禹,等.以树木年轮密度资料重建鄂尔多斯中部地区6至10月降水量的变化[J].西北农林科技大学学报(自然科学版),2013,41(8):96-102.
[20] 刘禹,史江峰,V.Shishov,等.以树轮晚材宽度重建公元1726年以来贺兰山北部5~7月降水量[J].科学通报,2004,49(3):265-269.
[21] 孙毓,王丽丽,陈津,等.利用兴安落叶松树轮最大晚材密度重建大兴安岭北部5~8月气温变化[J].科学通报,2012,57(19):1785-1793.
[22] Sun B,Liu Y,Lei Y,et al.Warm-induced aridification in eastern Inner Mongolia evidenced by tree rings[J].Dendrochronologia,2017,42:73-79.
[23] 丁爱军,肖生春,彭小梅,等.霸王(Sarcozygium xanthoxylon)灌木年轮记录的1902-2015年阿拉善荒漠中部气候干湿变化[J].中国沙漠,2018,38(2):401-409.
[24] 肖生春,陈小红,丁爱军.近现代阿拉善荒漠气候变化与环境演变机制研究进展[J].中国沙漠,2017,37(6):1102-1110.
[25] 范子昂,魏文寿,陈峰,等.树轮记录的腾格里沙漠东缘1775-2005年降水变化[J].中国沙漠,2012,32(4):996-1002.
[26] 梁尔源,邵雪梅,刘鸿雁,等.树轮所记录的公元1842年以来内蒙古东部浑善达克沙地PDSI的变化[J].科学通报,2007,52(14):1694-1699.
[27] 马龙,刘廷玺,寇志强,等.科尔沁沙地榆树生长与水文气象因子的关系及气候重建[J].冰川冻土,2007,29(5):802-807.
[28] 马龙,刘廷玺,冀鸿兰,等.科尔沁沙地1826年以来榆树树轮宽度年表的建立及降水重建[J].第四纪研究,2011,31(2):360-369.
[29] 赵国青.正蓝旗古榆树种群特征及林下植物多样性的研究[D].呼和浩特:内蒙古农业大学,2011.
[30] Holmes R L.Computer-assisted quality control in tree-ring dating and measurement[J].Tree-Ring Bulletin,1983,44(3):69-75.
[31] 赵守栋,江源,焦亮,等.ARSTAN程序和R语言dplR扩展包进行树轮年表分析的比较研究[J].生态学报,2015,35(22):7494-7502.
[32] 李宗善,刘国华,傅伯杰,等.不同去趋势方法对树轮年表气候信号的影响——以卧龙地区为例[J].植物生态学报,2011,35(7):707-721.
[33] 李金建,邵雪梅,李媛媛,等.树轮宽度记录的松潘地区年平均气温变化[J].科学通报,2014,59(15):1446-1458.
[34] 曹洁萍,迟道才,武立强,等.Mann-Kendall检验方法在降水趋势分析中的应用研究[J].农业科技与装备,2008(5):35-37.
[35] Chang M,Lee R.Objective double-mass analysis[J].Water Resources Research,1974,10(6):1123-1126.
[36] 曹受金,曹福祥,项文化.利用树木年轮重建赣南地区1890年以来2-3月份温度的变化[J].生态学报,2012,32(20):6369-6375.
[37] 时兴合,秦宁生,朱海峰,等.青海杂多大果圆柏年轮指示的公元1360-2005年5-6月最高气温变化[J].科学通报,2010,55(19):1924-1931.
[38] 肖丁木,秦宁生,李金建,等.树轮宽度所指示的川西色达7月平均最高温度变化[J].中国沙漠,2013,33(5):1536-1543.
[39] 马永永.近500年来亚洲干旱变化的树轮记录研究[D].北京:中国科学院大学,2016.
[40] Campbell L,Liu H B,Nolla H A,et al.Annual variability of phytoplankton and bacteria in the subtropical North Pacific Ocean at Station ALOHA during the 1991-1994 ENSO event[J].Deep Sea Research Part I Oceanographic Research Papers,1997,30(2):167-192.
[41] Raspopov O M,Dergachev V A,Kolström T.Periodicity of climate conditions and solar variability derived from dendrochronological and other palaeoclimatic data in highlatitudes[J].Palaeogeography,2004,209(1/2/3/4):127-139.
[42] 蒋德明,张娜,阿拉木萨,等.我国固沙植物抗旱性及基于水量平衡的沙地造林合理密度研究进展[J].西北林学院学报,2013,28(6):75-83.
[43] 赵丽,王晓江,刘果厚,等.浑善达克沙地榆树种群结构、格局及动态研究[J].中国沙漠,2009,29(3):508-513.