PROGRESS IN GEOGRAPHY ›› 2018, Vol. 37 ›› Issue (4): 485-494.doi: 10.18306/dlkxjz.2018.04.004
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Zhixin HAO1,2, Yani LIANG1,2, Yang LIU1,2, Xiu GENG1,2, Jingyun ZHENG1,2,*()
Received:
2018-02-03
Revised:
2018-03-20
Online:
2018-04-20
Published:
2018-04-20
Contact:
Jingyun ZHENG
E-mail:zhengjy@igsnrr.ac.cn
Supported by:
Zhixin HAO, Yani LIANG, Yang LIU, Xiu GENG, Jingyun ZHENG. Characteristics of temperature changes during the past millennium along the Ancient Silk Road[J].PROGRESS IN GEOGRAPHY, 2018, 37(4): 485-494.
Tab.1
Summary information of high-resolution proxy-based temperature reconstruction for the past millennium along the Ancient Silk Road"
序号 | 地区/点 | 代用证据 | 区域范围或 样点经纬度 | 样点海拔/m | 重建指标 | 温度变化解释方差 | 重建时段 | 时间分辨率/a | 来源 | |
---|---|---|---|---|---|---|---|---|---|---|
1 | 关中地区 | 历史文献 | 33.6oN~35.8oN, 106.3oE~110.6oE | 10-4月平均气温 | 35%(年际) | AD600-AD902 | 1~30 | Liu et al, 2016 | ||
2 | 西北地区 东部 | 历史文献 | 33.5oN~39.5oN, 102oE~112oE | 年平均气温 | 85%(30年 低通滤波) | AD960-AD1368 | 30 | 郝志新等, 2009 | ||
3 | 祁连山 中段 | 树轮宽度 | 38.43oN, 99.93oE | 3400-3550 | 12-4月平均气温 | 22%(年际) | AD900-AD2000 | 1 | Liu et al, 2005 | |
4 | 祁连山 | 树轮宽度 | 38.69oN~38.72oN, 99.67oE~99.70oE | 3300-3578 | 1-8月平均最低气温 | 59%(年际) | AD670-AD2012 | 1 | Zhang et al,2014 | |
5 | 阿尔泰山 | 树轮宽度,多个样点综合 | 45oN~50oN, 85oE~90oE | 6-8月平均气温 | 24%(年际) | AD104-AD2011 | 1 | Büntgen et al, 2016 | ||
6 | 别卢哈山 | 冰芯氧同位素(δ18O)含量 | 49.8oN, 86.6oE | 4062 | 3-11月平均气温 | 68%(年代际) | AD1250-AD2001 | 10 | Eichler et al, 2009 | |
7 | 土耳其西 南部 | 树轮碳同位素(δ13C)变化 | 36.6oN, 30.0oE, | 1850-2020 | 1-5月平均气温 | 27%(年际) | AD1125-AD2006 | 1 | Heinrich et al, 2013 | |
8 | 欧洲中部 | 树轮宽度,多个样点综合 | 40oN~50oN, 5oE~20oE | 6-8月平均气温 | 51%(年际);84%(60年低通滤波) | 500BC-AD2000 | 1 | Büntgen et al, 2011 | ||
9 | 欧洲大部 | 树轮、文献等多种证据集成 | 35oN~70oN, 10oW~40oE | 6-8月平均气温 | 66%(年至31年带通滤波) | 138BC-AD2003 | 1 | Luterbacher et al, 2016 |
Fig.2
Temperature variations during the past millennium along the Ancient Silk Road (a, c, e, f, g), and over China (b) and Asia (d) (a. Qilian mountain of Northwestern China (the mean of series 3 and 4 in Table 1); b. Synthesized reconstruction of China (Ge et al, 2013); c. Altai of Central Asia (slim-grey line: Series 5 in Table 1; thick-grey line: Series 6 in Table 1); d. Synthesized reconstruction of Asia (Shi et al, 2015); e. Southwestern Turkish (Series 7 in Table 1); f. Central Europe (Series 8 in Table 1); g. Most parts of Europe (Series 9 in Table 1); The temperature anomaly for all the series is relative to the mean of 1850-1950. Slim horizontal line: mean of the series; Bold line: 30-a fast Fourier (FFT) smoothing)"
Table 2
Cold and warm periods revealed by the summer temperature reconstruction series during the past 2000 years in Europe"
持续百年以上的冷暖期 | 暖期1 | 冷期1 | 暖期2 | 冷期2 | 暖期3 | 冷期3 | 20世纪暖期 |
---|---|---|---|---|---|---|---|
起讫时间/AD 温度距平/oC | 33-288 0.1 | 308-660 -0.2 | 670-1028 0.1 | 1029-1136 -0.3 | 1137-1251 0.3 | 1275-1860 -0.3 | 1901-2000 0.2 |
最暖百年/AD 温度距平/oC | 33-132 0.3 | 427-526 0.0 | 911-1010 0.3 | 1037-1136 -0.3 | 1137-1236 0.3 | 1353-1452 -0.1 | |
最暖30年/AD 温度距平/oC | 33-62 0.6 | 481-510 0.3 | 726-755 0.2 | 1077-1106 0.0 | 1141-1170 0.5 | 1400-1429 0.0 | 1924-1953 0.5 |
111-140 0.3 | 964-993 0.5 | 1198-1217 0.5 | 1532-1561 0.0 | 1985-2003 0.8 | |||
228-257 0.2 | 1752-1782 -0.1 | ||||||
最冷百年/AD 温度距平/oC | 138-237 -0.1 | 536-635 -0.4 | 773-872 -0.1 | 1032-1131 -0.3 | 1151-1250 0.3 | 1579-1678 -0.5 | |
最冷30年/AD 温度距平/oC | 150-179 -0.3 | 329-358 -0.5 | 796-825 -0.3 | 1029-1058 -0.4 | 1329-1358 -0.4 | 1955-1984 0.0 | |
536-565 -0.7 | 1107-1136 -0.5 | 1453-1482 -0.6 | |||||
1579-1608 -0.8 | |||||||
1672-1701 -0.6 | |||||||
1812-1841 -0.6 |
[1] | 陈发虎, 安成邦, 董广辉, 等. 2017. 丝绸之路与泛第三极地区人类活动、环境变化和丝路文明兴衰[J]. 中国科学院院刊, 32(9): 967-975. |
[Chen F H, An C B, Dong G H, et al.2017. Human activities, environmental changes, and rise and decline of Silk Road Civilization in Pan-Third Pole Region[J]. Bulletin of Chinese Academy of Sciences, 32(9): 967-975.] | |
[2] | 葛全胜. 2011. 中国历朝气候变化[M]. 北京: 科学出版社. |
[Ge Q S.2011. Climate change in Chinese dynasties[M]. Beijing, China: Science Press.] | |
[3] | 郝志新, 葛全胜, 郑景云. 2009. 宋元时期中国西北东部的冷暖变化[J]. 第四纪研究, 29(5): 871-879. |
[Hao Z X, Ge Q S, Zheng J Y.2009. Temperature variations during the Song and Yuan Dynasties (960-1368A. D.) in the eastern part of North West China[J]. Quaternary Sciences, 29(5): 871-879.] | |
[4] | 郝志新, 耿秀, 刘可邦, 等. 2017. 关中平原过去1000年干湿变化特征[J]. 科学通报, 62(21): 2399-2406. |
[Hao Z X, Geng X, Liu K B, et al.2017. Dryness and wetness variations for the past 1000 years in Guanzhong Plain[J]. Chinese Science Bulletin, 62(21): 2399-2406.] | |
[5] |
刘卫东. 2015. “一带一路”战略的科学内涵与科学问题[J]. 地理科学进展, 34(5): 538-544.
doi: 10.11820/dlkxjz.2015.05.001 |
[Liu W D.2015. Scientific understanding of the Belt and Road Initiative of China and related research themes[J]. Progress in Geography, 34(5): 538-544.]
doi: 10.11820/dlkxjz.2015.05.001 |
|
[6] | 荣新江. 2015. 丝绸之路与东西文化交流[M]. 北京: 北京大学出版社. |
[Rong X J.2015. Silk Road and cultural interaction between East and West[M]. Beijing, China: Peking University Press.] | |
[7] |
徐新良, 王靓, 蔡红艳. 2016. “丝绸之路经济带”沿线主要国家气候变化特征[J]. 资源科学, 38(9): 1742-1753.
doi: 10.18402/resci.2016.09.12 |
[Xu X L, Wang L, Cai H Y.2016. Spatio-temporal characteristics of climate change in the Silk Road Economic Belt[J]. Resources Science, 38(9): 1742-1753.]
doi: 10.18402/resci.2016.09.12 |
|
[8] |
Bianchi G G, McCave I N.1999. Holocene periodicity in North Atlantic climate and deep-ocean flow south of Iceland[J]. Nature, 397: 515-517.
doi: 10.1038/17362 |
[9] |
Büntgen U, Myglan V S, Ljungqvist F C, et al.2016. Cooling and societal change during the Late Antique Little Ice Age from 536 to around 660 AD[J]. Nature Geoscience, 9(3): 231-236.
doi: 10.1038/ngeo2652 |
[10] |
Büntgen U, Tegel W, Nicolussi K, et al.2011. 2500 years of European climate variability and human susceptibility[J]. Science, 331: 578-582.
doi: 10.1126/science.1197175 |
[11] |
Chen F H, Chen J H, Holmes J, et al.2010. Moisture changes over the last millennium in arid Central Asia: A review, synthesis and comparison with monsoon region[J]. Quaternary Science Reviews, 29(7-8): 1055-1068.
doi: 10.1016/j.quascirev.2010.01.005 |
[12] |
Chen Y N, Li Z, Li W H, et al.2016. Water and ecological security: Dealing with hydroclimatic challenges at the heart of China's Silk Road[J]. Environmental Earth Sciences, 75(10): 881.
doi: 10.1007/s12665-016-5385-z |
[13] |
Cook E R, Seager R, Kushnir Y, et al.2015. Old World megadroughts and pluvials during the Common Era[J]. Science Advances, 1(10): 1-9.
doi: 10.1126/sciadv.1500561 pmid: 4640589 |
[14] |
Diaz H F, Trigo R, Hughes M K, et al.2011. Spatial and temporal characteristics of climate in Medieval Times Revisited[J]. Bulletin of the American Meteorological Society, 92(11): 1487-1500.
doi: 10.1175/BAMS-D-10-05003.1 |
[15] |
Eichler A, Olivier S, Henderson K, et al.2009. Temperature response in the Altai region lags solar forcing[J]. Geophysical Research Letters, 36(1): L01808, doi: 10.1029/2008GL035930.
doi: 10.1029/2008GL035930 |
[16] |
Finné M, Holmgren K, Sundqvist H S, et al.2011. Climate in the eastern Mediterranean, and adjacent regions, during the past 6000 years: A review[J]. Journal of Archaeological Science, 38(12): 3153-3173.
doi: 10.1016/j.jas.2011.05.007 |
[17] |
Ge Q, Hao Z, Zheng J, et al.2013. Temperature changes over the past 2000 yr in China and comparison with the Northern Hemisphere[J]. Climate of the Past, 9(3): 1153-1160.
doi: 10.5194/cp-9-1153-2013 |
[18] |
Heinrich I, Touchan R, Liñán I D, et al.2013. Winter-to-spring temperature dynamics in Turkey derived from tree rings since AD 1125[J]. Climate Dynamics, 41(7-8): 1685-1701.
doi: 10.1007/s00382-013-1702-3 |
[19] | IPCC. 2013. Climate change 2013: The physical science basis. Contribution of working group I to the fifth assessment report of the Intergovernmental Panel on Climate Change[M]. Cambridge, New York: Cambridge University Press. |
[20] |
Jia D, Fang X Q, Zhang C P.2017. Coincidence of abandoned settlements and climate change in the Xinjiang oases zone during the last 2000 years[J]. Journal of Geographical Sciences, 27(9): 1100-1110.
doi: 10.1007/s11442-017-1424-2 |
[21] | Lamb H H.1977. Climate: Present, past and future, volume 2: Climatic history and the future[M]. London, UK: Methuen. |
[22] |
Li P Y, Qian H, Zhou W F.2017. Finding harmony between the environment and humanity: An introduction to the thematic issue of the Silk Road[J]. Environmental Earth Sciences, 76(3): 105.
doi: 10.1007/s12665-017-6428-9 |
[23] |
Li Z, Chen Y N, Wang Y, et al.2016. Drought promoted the disappearance of civilizations along the ancient Silk Road[J]. Environmental Earth Sciences, 75(14): 1116.
doi: 10.1007/s12665-016-5925-6 |
[24] |
Liu X H, Qin D H, Shao X M, et al.2005. Temperature variations recovered from tree-rings in the middle Qilian Mountain over the last millennium[J]. Science in China: Earth Sciences, 48(4): 521-529.
doi: 10.1360/03yd0063 |
[25] |
Liu Y C, Dai J H, Wang H J, et al.2016. Phenological records in Guanzhong area in central China between 600 and 902 AD as proxy for winter half-year temperature reconstruction[J]. Science China: Earth Sciences, 59(9): 1847-1853.
doi: 10.1007/s11430-016-5325-5 |
[26] | Luterbacher J, García-Herrera R, Akcer-On S, et al.2012. A review of 2000 years of Paleoclimatic evidence in the Mediterranean[M]//Lionello P. The climate of the mediterranean region: From the past to the future. Amsterdam, Netherlands: Elsevier: 87-185, doi: 10.1016/B978-0-12-416042-2.00002-1. |
[27] |
Luterbacher J, Werner J P, Smerdon J E, et al.2016. European summer temperatures since Roman times[J]. Environmental Research Letters, 11(2): 024001, doi: 10.1088/1748-9326/11/2/024001.
doi: 10.1088/1748-9326/11/2/024001 |
[28] |
PAGES 2k Consortium.2013. Continental-scale temperature variability during the past two millennia[J]. Nature Geoscience, 6(5): 339-346.
doi: 10.1038/ngeo1797 |
[29] |
PAGES 2k Consortium, 2017. A global multiproxy database for temperature reconstructions of the Common Era[J]. Scientific Data, 4: 170088, doi: 10.1038/sdata.2017.88.
doi: 10.1038/sdata.2017.88 pmid: 5505119 |
[30] |
Patterson W P, Dietrich KA, Holmden C, et al.2010. Two millennia of North Atlantic seasonality and implications for Norse colonies[J]. Proceedings of the National Academy of Sciences of the United States of America, 107(12): 5306-5310.
doi: 10.1073/pnas.0902522107 pmid: 20212157 |
[31] |
Shi F, Ge Q S, Bao Y, et al.2015. A multi-proxy reconstruction of spatial and temporal variations in Asian summer temperatures over the last millennium[J]. Climatic Change, 131(4): 663-676.
doi: 10.1007/s10584-015-1413-3 |
[32] |
Touchan R, Akkemik Ü, Hughes M K, et al.2007. May-June precipitation reconstruction of southwestern Anatolia, Turkey during the last 900 years from tree rings[J]. Quaternary Research, 68(2): 196-202.
doi: 10.1016/j.yqres.2007.07.001 |
[33] |
Zhang Y, Shao X M, Yin Z Y, et al.2014. Millennial minimum temperature variations in the Qilian Mountains, China: Evidence from tree rings[J]. Climate of the Past, 10(5): 1763-1778.
doi: 10.5194/cpd-10-341-2014 |
[34] |
Zhang Y, Tian Q H, Gou X H, et al.2011. Annual precipitation reconstruction since AD 775 based on tree rings from the Qilian Mountains, northwestern China[J]. International Journal of Climatology, 31(3): 371-381.
doi: 10.1002/joc.2085 |
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