[1]陈隆勋,朱乾根,罗会邦,等.东亚季风[M].北京:气象出版社,1991:1-262. [2]Yeh D H.Some characteristics of the summer circulation over the Tibetan Plateau and its neighborhood[J].Bull Am Meteor Soc,1981,62:14-19. [3]Manabe S,Terpstra T B.The effects of mountains on the general circulation of atmosphere as identified by numeral experiments[J].J Atmos Sci,1974,31:3-42. [4]屈文军,张小曳,王丹,等.西风带研究的重要意义[J].海洋地质与第四纪地质,2004,24(1):125-132. [5]Visbeck M.The ocean’s role in Atlantic climate variability[J].Science,2002,297:2223-2224. [6]Porter S C,An Z S.Correlation between climate event in the North Atlantic and China during the last glaciation[J].Nature,1995,375:305-308. [7]Chen F H,Bloemendal J,Feng Z D,et al.East Asian monsoon variations during the last interglacial: Evidence from the north western margin of the Chinese loess plateau[J].Quaternary Science Reviews,1999,18(8-9):1127-1135. [8]Bond G,Showers W,Cheseby M,et al.A pervasive millennial-scale cycle in north Atlantic Holocene and glacial climates[J].Science,1997,278:1257-1266. [9]周卫建,卢雪峰,武振坤,等.若尔盖高原全新世气候变化的泥炭记录与加速器放射性碳测年[J].科学通报,2001,46(12):1040-1044. [10]王华,洪业汤,朱咏煊,等.青藏高原泥炭腐值化度的古气候意义[J].科学通报,2004,49(7):686-691. [11]陈发虎,朱艳,李吉均,等.民勤盆地湖泊沉积记录的全新世千百年尺度夏季风快速变化[J].科学通报,2001,46(17):1414-1419. [12]施雅风,孔昭宸,王苏民,等.中国全新世大暖期的气候与环境的基本特征[C]∥施雅风主编.中国全新世大暖期气候与环境[M].北京:海洋出版社,1992:1-18. [13]陈发虎,吴薇,朱艳,等.阿拉善高原中全新世干旱事件的湖泊记录研究[J].科学通报,2004,49(1):1-9. [14]覃嘉铭,袁道先,程海,等.新仙女木及早中全新世气候突变事件:贵州茂兰石笋氧同位素记录[J].中国科学:D辑,2004,34(1):69-74. [15]钟巍,王立国,熊黑钢,等.塔里木盆地南缘和田绿洲中全新世以来气候环境变化与人类活动[J].中国沙漠,2007,27(2):171-176. [16]李琼,潘保田,高红山,等.腾格里沙漠南缘末次冰盛期以来沙漠演化与气候变化[J].中国沙漠,2006,26(6):875-879. [17]弋双文,鹿化煜,周亚利,等.晚第四纪科尔沁沙地干湿变化的黄土记录[J].中国沙漠,2006,26(6):869-874. [18]史正涛,宋友桂,安芷生.天山黄土记录的古尔班通古特沙漠形成演化[J].中国沙漠,2006,26(5):675-679. [19]张洪,靳鹤龄,苏志珠,等.全新世浑善达克沙地粒度旋回及其反映的气候变化[J].中国沙漠,2005,25(1):1-7. [20]李明启,靳鹤龄,董光荣,等.萨拉乌苏河流域微量元素揭示的气候变化[J].中国沙漠,2006,26(2):172-179. [21]袁宝印,魏兰英,王振海,等.新疆巴里坤湖十五万年来古水文演化序列[J].第四纪研究,1998,18(4):319-327. [22]李吉均.中国西北地区晚更新世以来气候变迁模式[J].第四纪研究,1990,10(3):197-203. [23]韩淑媞,袁玉江.新疆巴里坤湖35000年来古气候变化序列[J].地理学报,1990,45(3):350-362. [24]韩淑媞.北疆巴里坤湖全新世环境变迁序列[J].地质科学,1992(增刊):247-260. [25]韩淑媞,王承义,袁玉江.北疆干旱区500年来环境演变序列[J].中国沙漠,1992,12(1):1-8. [26]Stuiver M,Reimer P J,Reimer R.CALIB Radiocarbon Calibration[R/OL].[2006-02-10][ 2006-10-20].http://calib.qub.ac.uk/calib/. [27]张成君,曹洁,类延斌,等.中国新疆博斯腾湖全新世沉积环境年代学特征[J].沉积学报,2004,22(3):494-499. [28]Hakanson L,Jansson M.Principles of Lake Sedimentology[M].Berlin:Springer,1983:242-316. [29]孙千里,周杰,肖举乐.岱海沉积物特征及其古环境意义[J].海洋地质与第四纪地质,2001,21(1):93-95. [30]钟巍,王立国,塔西甫拉提·特依甫,等.太阳活动对塔里木盆地南缘近4ka以来气候波动的可能影响[J].科学通报,2004,49(11):1079-1083. [31]Alley R,Mayewski P,Sowers T,et al. Holocene climatic instability: A prominent,widespread event 8200 years age[J].Geology,1997,25(6):483-486. [32]吴海斌,郭正堂.末次盛冰期以来中国北方干旱区演化及短尺度干旱事件[J].第四纪研究,2000,20(6):548-558. [33]吴敬禄.新疆艾比湖全新世沉积特征及古环境演化[J].地理科学,1995,15(1):39-46. [34]GRIP members. Climate instability during the interglacial period recorded in GRIP ice core[J].Nature,1993,364:203-207. [35]Sirocko F,Sarnthein M,Erlenkeuser H.Century-scale events in monsoonal climate over the past 24000 years[J].Nature,1993,364:322-32. [36]汪卫国,冯兆东,李心清,等.蒙古北部Gun Nuur湖记录的全新世气候突发事件[J].科学通报,2004,49(1):27-33. [37]竺可桢.中国近五千年来气候变迁的初步研究[J].中国科学,1973(2):168-189. [38]许靖华.太阳、气候、饥荒与民族大迁移[J].中国科学:D辑,1998,28(4):366-384. [39]Schulza M,Mudelsee M.REDFIT:estimating red-noise spectra directly from unevenly spaced paleoclimatic time series[J].Computers & Geosciences,2002,28:421-426. [40]Stuiver M,Braziunas T.Sun,ocean,climate and atmospheric 14CO2:An evaluation of causal and spectral relationships[J].Holocene,1993,3 (4):289-305. [41]Gleissberg W.A table of secular variations of the solar cycle[J].Terrestrial Magnetism and Atmospheric Electricity,1994,49:243-244. [42]Ram M,Stolz M R.Possible solar influence on the dust profile of GISP2 ice core from central Greenland[J].Geophysical Research Letters,1999,26:1043-1046. [43]Dean W E. Rates,timing and cyclicity of Holocene eolian activity in north-central United States-evidence from varied lake sediment[J].Geology,1997,25:331-334. [44]Campbeell I D,Campbell C,Apps M J,et al.Late Holocene—1500years climatic periodicities and their implications[J].Geology,1998,26:471-473. [45]Sirocko F,Garbe S D,McIntyre A,et al.Teleconnections between the subtropical monsoon and high-latitude climates during the last deglaciation[J].Science,1996,272:526-529. [46]陈发虎,黄小忠,杨美林,等.亚洲中部干旱区全新世气候变化的西风模式[J].第四纪研究,2006,26(6):881-887. [47]Bond G,Kromer B,Beer J,et al.Persistent solar influence on North Atlantic climate during the Holocene[J].Science,2001,294:2130-2136. [48]Bianchi G G,McCave I N. Holocene periodicity in north Atlantic climate and deep-ocean flow south of Iceland[J].Nature,1999,397:515-517. [49]Zhou W J,Head M J,Lu X F,et al.Teleconnection of climatic events between east Asia and polar high latitude areas during the last deglaciation[J].Paleogeography,Paleoclimatology,Paleoecology,1999,152:163-172. [50]Charles C.The ends of an era[J].Nature,1998,394:422-423. |