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==== O = N O M M S N #$% Vol.2, No. 1 January, 2 0 0 6 ADVANCES IN CLIMATE CHANGE RESEARCH 1673-1719 (2006) 01-0021-07 #$%&'() New Advances in Research on the Little Ice Age Climate Change NIO == P OIP O N= = #$%&= #$%& #$%&==TPMMOM O=!= #$%&'= #$%&' () =TPMMMM P= = #$%&'( #$%&'==TPMMMM = #$%&'()*+,-./0123456789:;.<=! #$%&'() * # 500 a (1400J1900 AD) #$%& L! #$%& # #$%&'()* #$%&! #$%&'()*+ #$%&'()* +,-./0(12345 #$ #$%&'()*!+,!! #P467==== #A = ==== 3 #$%&'()*+ 500 a #$%&'() #$%&'()* 4 # #$%&'() #$ #$%& #$%&'()*+, #$%&'( Little Ice Age LIA! Matthes 1 #$%&'()*"+ #$%&'()#* 2 #$%&'! 1000 a #$%&'(!! #$% 3 = #$%&'! *+,-./012 #$%&'()*+,-. 5J9 10J14 #$%&'()*+ #$% ==== #$%&'()*+,-./01 #$%&'()*+%,-. #$%&' 15 #$%&'()*+,-./01 1992 #$%&'()*+ 1000 a #$%&'()*+! 2005J09J14 = 2005J12J06 #$%&!'()%&!*+'(,- IAM200413 1968J! L #$%&'( 2002CSB #$%&' K=E-mail: wangjs02@lzu.edu.cn Adv. Clim. Change Res., 2006, 2 ( 1): 21-27 #$% #$%& ========= 20020730010 # 500 a #$% #$%

==== 22 #$% =OMMS! #$ 10 a #$%& #$%&'( #$%& #$%&'()*+,-./ N==! if^ NKN== ==== #$%&' 16 #$% #1400J1500AD1600J1700AD #$1650 30AD #$ 17 #$%&'()! 18 #!$%&'()* #"$ 1780J1920AD #$%&'()"* #$%&'() 19 #$% 0.5 #$%&'()! #$%&'()*&+,-. 8 #$%& 14J19 #$% NKO== ====Stuiver et al. 20 # GISP2 18 O #$% # 1350J1800AD Jensen et al. 6 # GRIP 1300J1900AD #$%& #$%&'"()$*+,-! #$% #$%&'() 21 #$%& 22 3 #$ 1200J1300AD1610J1750AD1870J1900AD 23 #$%& 1300J1850AD #$%&'()* #$%&'()*+, ==== #$%&'()*+,-./ O Hara et al. 24 # 1640J1915AD #$%&'() #$%&' #$%&' #$%&%'( # 7 #$%&'( 25J26 #$%& #$%&'()*+,- #! NKP== ==== #$%& #$%&'( #!$%& # 27 600200 abp # 28! #$%&'()*+ Repinski et al. 29 #$%& #$%I #$%&'()*+ #$%&'()1700AD #$! 30 #$%&'()*+,-I! L #$% NKQ== ==== #$%&'()*+1300J1900AD #$%&'( 31 #$%&! #$%&'( 32! 3!1400J1500AD1600J1700AD 1850J 1920AD!#$8 #$%! 420 a #$%&'(&$ 9!# #$%&'()!#$% #$ 1870 #$% #$%#&'()*+ NKR== ==== #$%&'()*+,-./01! 10 #$%&! 11 14! 33 #$Yang et alk 34 #2000 a 1400AD # 1920AD 17 1000 a #$ # #$%&'()*+,-./! #$%&'()*+%, # #$%& 35 #$% 18 O NP C PS 3 # 1545J 1640AD1675J1745AD 1790J1825AD 1475J1690AD!1690J1825AD! #$%&' 37 #$%&'! 12 #$%&'()*+,

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==== 24 #$% =OMMS #$%& 500 a1400j1900ad #$ #$%&'! #$%&' #$%! #$%& #$%& #$% #$%&'() ==== #$% #$%&'(3 #$%&'(17 #$%&'() #$%&'! #$%&'()*+ OKP==if^ #$ ==== #$%&'()*+ #$%&!'() #$$% #$%&'()*+,-. 18 O 13 #$ # #$ #$% #$%&' #$%&'() 17 200 mm18! # 210 mm19 # #$%&'()*+,-! # 180 mm! 50! #$%&' #$%&' 51 #$%&' #$% #$%&&'()*+, # #$%&'()*+ #$% #$%&'() #$% #$% 52J53 # ==== #$%&'()&*Winter=et al. 54 # #!#$%& 23 1300J1850AD #$%& #$%&'()*+,-34 55 #$%&'()*)1450J1530AD 1720J1850AD #$%&'( 24 56 1430J1670AD #$% #$%& 0.8 57 Tyson et al. 30 # #$%&"' 1 #$%&'()*+,-. #$% 0.5 19 #$%& 58 20 #$1 #$%&'()*+20 # 1.52 58 ==== #$ #$%&'()! #$%&' #$%& #$%2 #$%&4 #$ #$%&'! #$% #$%&'($) * #$! # 1 #$ P==if^ #$ ==== #$%&'()*+,-./01 # 59 #$%&'( 60 Jones et al. 61 #$ ENSO #$%NAO # 5 #$%& #$%&'()*+ #$% #$%&'()*+,-./012(! 62 #$%&'()*+,- THC 56 THC # #$%& ==== #$ #$%&'() #$%&'()*+,- 63! I #$%&'()*I # 51 #$%&'()*! # #$%& #$ #$%&' ==== #$%&'()*#+ #$%&'()* #$%& #$ %&' #$% #$%&'() # #$%!&'() #$% #$ #$%& # #$%&'()*+,-./012 #$%&'"() #$%& #$%&'()*+,-./

N!W #$%&'() 25 Q=== ===1 #$%&'()*+,-./ #$%&'()* +,-! #$% #$ #$%&'()*+,-./01 # #$%&'()*+ 1000 a #$% ===2 #$%&'()*+,- #$%&'()*+',-./ #$%&'()*+,-. # #$%&'()*+ #$%&'()* #$%& #$%& ===P #$%&'()*+,"-. #$% # #$%&'()*+,-./$01 ===Q #L #L! #$%&'()*+ #$%&'()*+,-./0123 #$%&'()* # #$%&'()*+ ===R #$%&'()* #$%& #$%&'()* #$%&'() #$%&' #$%&!'() #$%& #$%& [3] [4] [5] [6] [7] [8] [9] [10] [11] [12] [13] [14] [15] Mikami T. Proceedings of the International Symposium on the Little Ice Age Climate [C]. Tokyo: Tokyo Metropolitan University, 1992: 1-5,141-174, 253-277. K #$%&'()*+,-./0123456 [J]. #2001, 24 ( 1): 67JTPK Kreutz K J, Mayewski P A, Meeker L D, et al. Bipolar changes in atmospheric circulation during the Little Ice Age [J]. Science, 1997, 277:1294-1296. Jensen D D, Mosegaard K, Gundestrup N, et al. Past temperatures directly from the Greenland ice sheet [J]. Science, 1998, 282: 268-271. Haug G H, Hughen K A, Sigman D M, et al. Southward migration of the intertropical convergence zone through the Holocene [J]. Science, 2001, 293:1304-1308. McDermott F, Mattey D P, Hawkesworth C. Centennial-scale Holocene climate variability revealed by a high-resolution speleothem δ 18 O record from SW Ireland [J]. Science, 2001, 294:1328-1331. Hendy E J, Gagan M K, Alibert C A, et al. Abrupt decrease in tropical Pacific sea surface salinity at end of Little Ice Age [J]. Science, 2002, 295:1511-1514. K= RMMM #$%&'(=[J].!B FI=1973, 16 (2): 291J296K I= I= K= #$%=[J].= I 1998, 18 (1): 54J62K I= I===I=K= #$ %&'()[J].!EB FI=1990, 20 (11):1196J1201K I= I= I= K= #$!%&'()* [J].=!EB FI=1995, 25 (10): 1108J1114K K= #$%&'()*+, -. [J].=! I=1991, 11(2): 104J111K Jones P D, Briffa K R. Preface: The Little Ice Age : Local and global perspectives [J]. Climate Change, 2001, 48(1): 5-8. #$%&'()*+,-./012)3 #$%&' #$% #$! #$! [1] Matthes F E. Report of the committee on glaciers, transactions of the America [J]. Geophysical Union, 1939, 20: 518-523. [2] Lamb H H. Climate: Present, Past and Future [M]. London: Methuen, 1977: 100, 221, 430. [16] Bodri L, Cermak V. Climate change of the last millennium inferred from borehole temperatures: regional patterns of climatic changes in the Czech Republic-part III [J]. Glob. and Planet. Change, 1999, 21: 225-235. [17] Matthews J A, Dahl S O, Nesje A, et al. Holocene glacier variations in central Jotunheimen, southern Norway based on distal glaciolacustrine sediment cores [J]. Quat. Sci. Rev., 2000, 19: 1625-1647. [18] Jennings A E, Hagen S, Hardardottir J, et al. Oceanographic change and terrestrial human impacts in a post AD1400 sediment record from the Southwest Iceland shelf [J]. Climate Change, 2001,48(1): 83-100. [19] Brooksa S J, Birks H J B. Chironomid-inferred air temperatures from

==== OS #$% =OMMS Lateglacial and Holocene sites in north-west Europe: progress and problems [J]. Quaternary Science Reviews, 2001, 20:1723-1741. [34] Yang B, Braeuning A C, Johnson K R. General characteristics of temperature variation in China during the last two millennia [J]. [20] Stuiver M, Grootes P M, Baraziunas T F. The GISP2 δ 18 O climate Geophysical Research Letters, 2002, 29 (9): 381-384. record of the past 16500 years and the role of the sun, ocean and volcanoes. [J]. Quaternary Research, 1995, 44: 341-354. [35] Tan M, Liu T S, Hou J Z, et al. Cyclic rapid warming on centennial-scale revealed by a 2650-year stalagmite record of warm season temperature [21] Nederbragt A J, Thurow J W. A 6000 year varve record of Holocene [J]. Geophysical Research Letters, 2003, 30 (12): 191-194. climate in Saanich Inlet, British Columbia, from digital sediment colour [36] Paulsen D E, Li H C, Ku T L. Climate variability in central China over analysis of ODP Leg 169S cores [J]. Marine Geology, 2001, 174: 95- the last 1270 years revealed by high-resolution stalagmite records [J]. 110. Quaternary Science Reviews, 2003, 22: 691-701. [22] Calkin P E, Wiles G C, Barclay D J. Holocene coastal glaciation of Alaska [37] I= I= K= #$%&'( [J].= [J]. Quaternary Science Reviews, 2001, 20: 449-461. =ED FI=1996, 26 (5): 474J480K [23] Nyberg J, Kuijpers A, Malmgren B A, et al. Late Holocene changes in [38]!! K= #$%&'()*+=[J].= precipitation and hydrography recorded in marine sediments from the Northeastern Caribbean Sea [J]. Quaternary Reesarch, 2001, 56: 87-102. [39]!2001, 26 (24): 2069J2073K I K= #$%&'()*+,-./+01 [24] O Hara S L, Metcalfe S E. The climate of Mexico since the Aztec period [J].! I=2002, 24 (3): 234J244K [25] [26] [27] [28] [29] [30] [31] [32] [33] [J]. Quaternary International, 1997, 43: 1-7. Goodman A Y, Rodbell D T, Seltzer G O, et al. Subdivision of glacial deposits in Southeastern Peru based on pedogenic development and radiometric ages [J]. Quaternary Research, 2001, 56: 31-50. Cioccale M A. Climatic fluctuations in the central region of Argentina in the last 1000 years [J]. Quaternary International, 1999, 62: 35-47. Huffman T N. Archaeological evidence for climatic change during the last 2000 years in Southern Africa [J]. Quaternary International, 1996, 33: 55-60. Stager J C, Cumming B, Meeker L. A high-resolution 11400-yr diatom record from Lake Victoria, East Africa [J]. Quaternary Research, 1997, 47: 81-89. Repinski P, Holmgren K, Lauritzen S E, et al. A late Holocene climate record from a stalagmite, Cold Air Cave, Northern Province, South Africa [J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 1999, 150: 269-277. Tyson P D, Karlen W, Holmgren K, et al. The Little Ice Age and medieval warming in South Africa [J]. South African Journal of Science, 2000, 96: 121-126. Winkler S. The Little Ice Age maximum in the Southern Alps, New Zealand: Preliminary results at Mueller Glacier [J]. The Holocene, 2000, 10: 643-647. Hendy C H, Wilson A T. Palaeoclimate data from speleothems [J]. Nature, 1968, 219: 48-51. I I K #"$%&'(=[J].! I 2003, 15 (4): 369J376K [40] Tagami Y. Some remarks on the climate in the Medieval Warm Period of Japan [C] // Paleoclimate and environmental variability in Austral-Asian transect during the past 2000 years (IGBP Proceedings). Nagoya, Japan: Nogoya University, 1996: 115-119. [41] Kitagawa H, Matsumoto E. Climatic implications in a Japanese cedar (Cryptomeria japonica) during the last two millennia [J]. Geophys. Res. Lett., 1995, 22 (16): 2155-2188. [42] Narama C. Late Holocene variation of the Raigorodskogo Glacier and climate change in the Pamir-Alai, central Asia [J]. Catena, 2002, 48: 21-37. [43] Jacoby G C, Lovelius N V, Shumilov O I, et al. Long-term temperature trends and tree growth in the Taymir region of Northern Siberia [J]. Quaternary Research, 2000, 53: 312-318. [44] D Arrigo R, Jacoby G, Pederson N, et al. Mongolian tree-rings, temperature sensitivity and reconstructions of Northern Hemisphere temperature [J]. The Holocene, 2000, 10: 669-672. [45] Khim B K, Yoon H I, Kang C Y, et al. Unstable climate oscillations during the late Holocene in the Eastern Bransfield Basin, Antarctic Peninsula [J]. Quaternary Research, 2002, 58: 234-245. [46] Domack E W, Leventer A, Dunbar R, et al. Chronology of the Palmer Deep site, Antarctic Peninsula: A Holocene palaeoenvironmental reference for the circum-antarctic [J]. The Holocene, 2000, 11: 1-9. [47] Broecker W S. Was the medieval warm period global? [J]. Science, 2001, 291: 1497-1499. [48] Soon W, Baliunas S, Idso C, et al. Reconstructing climate and environmental changes of the past 1000 years: a reappraisal [J]. Energy

!W #$%&'() N 27 [49] [50] and Environment, 2003, 14 (2/3): 233-299. Mann M E, Bradley R S, Hughes M K. Global-scale temperature patterns and climate forcing over the past six centuries [J]. Nature, 1998, 392: 779-787. I= I= K=1000 #$%&'()*+, Ice Age and 20th century temperature variability from Chesapeake Bay [J]. Global and Planetary Change, 2003, 36: 17-29. [57] Williams P W, Marshall A, Ford D C, et al. Palaeoclimatic interpretation of stable isotope data from Holocene speleothems of the Waitomo district, North Island, New Zealand [J]. The Holocene, 1999, 9(2): 649-657. #$%&!'()=[J].= 2004, 49 (1): 22J [58] K= #$%[J].= I1995, 15 (3): 202J212K [51] [52] [53] [54] [55] [56] 26K I I I K= #$%=[J]. # I 2004, 14 (4): 462J468K I= K= #$%&'()*+ 4000!! [J].=!ED FI=1997, 27 (4): 366J372K I= I= I= K= #$%&'()*+ #EFW= #$=[J].=!D FI=2000, 30 (3): 239J248K Winter A, Ishioroshi H, Watanabe T, et al. Carribean sea surface temperatures: Two-to-three degree cooler than present during the Little Ice Age [J]. Geophysical Research Letters, 2000, 27: 3365-3368. demenocal P, Ortiz J, Guilderson T, et al. Coherent high- and low-latitude climate variability during the Holocene warm period [J]. Science, 2000, 288: 2198-2202. Cronin T M, Dwyer G S, Kamiya T, et al. Medieval Warm Period, Little [59] Lamoureux S F, England J H, Sharp M J, et al. A varve record of increased Little Ice Age rainfall associated with volcanic activity, Arctic Archipelabo, Canada [J]. The Holocene, 2001, 11: 243-249. [60] Stuiver M, Braziunas T F, Grootes P M, et al. Is there evidence for solar forcing of climate in the GISP2 oxygen isotope record? [J]. Quaternary Research, 1997, 48: 259-266. [61] Jones P D, Osborn T J, Briffa K R. The evolution of climate over the last millennium [J]. Science, 2001, 292: 662-667. [62] Qian W H, Zhu Y F. Little Ice Age climate near Beijing, China, inferred from historical and stalagmite records [J]. Quaternary Research, 2002, 57: 109-119. [63] Frenzel B, Galli M, Nanni T, et al. Solar output and climate during the Holocene [C] // 14th EPC/ESF Workshop. Stuttgart: Fischer, 1995: 131-160.! #$%&' ==== #$%&' #$!%"& ' #$%&'( #$%&'()* #$%&'#()*+,-./012 #$%& # #$%&'()*+ #$%&'( #$%&'()* #$%&'()*+,K= #! #$ #$ #$ #$! K ==== #$%&' #$%&'()* #$%&'()*+,-. #$%&'()*+,-.$/0123K ==== # #!6 12 72 K=! # K= 80J463K # #$%&'() 46 #$%&' ==100081! ===== L 010J58995171 E-mail: accr@cma.gov.cn http://