CLIMATIC VARIATIONS IN CHINA OVER THE LAST 2000 YEARS

YANG Bao; SHI Ya-feng; LI Heng-peng

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YANG Bao, SHI Ya-feng, LI Heng-peng. CLIMATIC VARIATIONS IN CHINA OVER THE LAST 2000 YEARS[J]. Chinese Geographical Science, 2001, 11(2): 97-103.

Citation:

YANG Bao, SHI Ya-feng, LI Heng-peng. CLIMATIC VARIATIONS IN CHINA OVER THE LAST 2000 YEARS[J]. Chinese Geographical Science, 2001, 11(2): 97-103.

CLIMATIC VARIATIONS IN CHINA OVER THE LAST 2000 YEARS

1.
Cold and And Regions Environmental and Engineering Research Institute, the Chinese Academy of Sciences, Lanzhou 730000, P. R. China;
2.
Institute of Geography and Limnology, the Chinese Academy of Sciences, Nanjing 210008, P. R. China

Funds: Under the auspices of the KZCX2-304 and KI 951-A1-202-04 Project of the Chinese Academy of Sciences.

Received Date: 2001-02-13
Publish Date: 2001-06-20

Abstract

A compilation of paleoclimate records from ice core, tree-rings, lake sediments and historical documents provides a view of temperature change in China over the recent 2000 years. For all-China temperature reconstruction, six sub-stages are identified for the last two millennia. Around AD 0-240, AD 800-1100, AD 1320-1400 and the period from AD 1880 on were warm while around AD 240-800, AD 1100-1320, AD 1400-1880 were cold. Also, temperature varied from region to region in each of the warm or cold periods. The Eastern Han warm period (0-AD 240), the cold period covering the span of Wei, Jin, and the Southern and Northern Dynasties, the MWP (AD 800-1100) and succeeding LIA occurred in eastern China and the Qilian Mountains. Only the fint two climatic events were recorded in Guliya ice core while the so-called MWP and LIA was far weaker. Also, the warming between AD 800 and 1100 didn't occur in the south of Xizang (Tibet) Plateau. Instead, the southern Xizang Plateau experienced warming in AD 1150-1400. The aggregated China temperature agrees well with North-hemisphere temperature in the past millennia, indicating close relationship of temperature changes between China and North-hemisphere.
- climatic variations,
- the last two millennia,
- China

References

[1]	BRADLEY R S,. JONES P D, 1993. 'Little Ice Age' summer temperature variations: their nature and relevance to recent global warming trends [J]. The Holocene, 3: 367-376.
[2]	BRAEUNING A, 1999. Zur Dendroklimatologie Hochtibets wahrend desletzten Jahrtausends [C]. Dissertationes Botanicae.
[3]	BRIFFA K R, 2000. Annual climate variability in the Holocene: interpreting the message of ancient trees [J]. Quaternary Science Reviews, 19: 87-105.
[4]	CROWLEY T J, LOWERY T S, 2000. How warm was the Medieval .Warm Period [J]. Ambio, 29(1): 51-54.
[5]	FUKUSAWA H, 1995. High-resolution reconstruction of environmental changes from the last 2000 years varied sediments in Lake Suigetsu central Japan [A]. In: Paleoclimate and Environmental Variability in AustraGAsianTransect during the Past 2000 Years [C], (Proceedings of the 1995 Nagoya IGBP-PAGES/PEP-Ⅱ Symposium) Nagoya University. Nagoya, Japan,84-89.
[6]	HONG Ye-tang, JIANG Hong-bo et al., 2000. Response of climate to solar forcing recorded in a 6000-year δ¹⁸O time-series of Chinese peat cellulose [J]. The Holocene, 10 (1): 1-7.
[7]	HUGHES M K, DIAZ H F, 1994. Was there a 'Medieval Warm Period', and if so, where and when [J]. Climatic Change, 26(2): 109-142.
[8]	INOUCHI Y, YOKOTA S, TERASHIMA S, 1995. Climatic changes around Lake Biwa during the past 300 000 years anc 2000 years [A]. In: Paleoclimate and Environmental variability in Austral-Asian Transect during the Past 2000 Yean [C] (Proceedings of the 1995 Nagoya IGBP-PAGES/PEP-Ⅱ Symposium). Nagoya University, Nagoya, Japan, 109-114.
[9]	JONES P D, BRADLEY R S, 1992. Climatic variations over thc last 500 years [A]. In: BRADLEY R S, JONES P 1: (eds.). Climate since A. D. 1500 [C]. London: Routledge, 649-665.
[10]	JONES P D, BRIFFA K R, Barnett T P et al., 1998.High-resolution palaeoclimatic records for the last millennium:Interpretation, integration and comparison with General Circulation Model control-run temperatures [J]. The Holocene, 8: 455-471.
[11]	JONES P D, OSBORN T J, BRIFFA K R, 1999. Estimatinl sampling errors in larger-scale temperature averages [J].Journal of Climate, 10: 2548-2568.
[12]	KANG Xing-cheng, GRAUMLICH L J, SHEPPARD P R, 1997.The last 1835 years climate changes inferred from tree rinl records in Dulan region, Qinghai, China [JI . Quaternar:Sciences, 1 : 70-75.
[13]	KITAGAWA H, 1995. Climatic implications in a Japanese ceda (Crhptomeria Japonica) during the last two millennia [J].Geophys. Res. Lett., 22(16): 2155 -2188.
[14]	LAMB H H, 1965. The early Medieval Warm Epoch and its se. quel [J]. Palaeogeography, Palaeoclimatology, Palaeoe cology, 1: 13 -37.
[15]	LIN Xue-chun, Yu Shu-qiu, TANG Guo-li, 1995. Series of av. erage air temperature over China for the last 100-year period [J].Scientia Atmspherica Sinica, 19(5): 525 -534. (in Chinese)
[16]	Lou Jian-yu, CHEN Zheng-dong, WANN J K, 1997. Paleocli. matological records of Great Ghost Lake in Taiwan [J]. Sci. . ence in China (Series D), 40(3): 284-292.
[17]	Lou Jian-yu, CHEN Zheng-dong, 1997. Paleoclimatological an(paleoenvironmental records since 4000 a B. P. in the sedi. ments of alpine lakes in Taiwan [J]. Science in China (Serie D), 40(4): 424 -431. hANN M E, BRADLEY R S, HUGHES M K, 1999. Northern hemisphere temperatures during the past millennium: 'Inferences, uncertainties, and limitations [J]. Geophys. Res.Lett., 26: 759-762.
[18]	IVERPECK J, HUGHEN K, HARDY D, et al., 1997. Arctic environmental changes of the last four centuries [J]. Nature, 278(5341): 1251-1256.
[19]	AKAGUCHI Y, 1983. Warm and cold stages in the past 7600 years in Japan and their global correlation-Especially on climatic to the global sea level changes and the ancient Japanese history [J]. Bulletin of Department of Geography,University of Tokyo, 15: 1-31.
[20]	SHI Ya-feng, YAO Tan-dong, YANG Bao, 1999. Decadal' climatic variations recorded in Guliya ice core and comparison with the historical documentary data from East China during the last 2000 years [J]. Science in China (Series D), 42 (Supplement): 91-100.
[21]	ANG Lin-yu, SHEN Cai-ming, LIU Kam-biu et al., 2000.Changes in south Asian monsoon: New high-resolution paleoclimatic records from Tibet, China [J]. Chinese Science Bulletin, 1: 87-91.
[22]	HOMPSON L G, MOSLEY-THOMPSON E, DAVIS M E et al., 1993. Recent Warming: Ice core evidence from tropical ice cores with emphasis on Central Asia [J]. Global Planet.Change, 7: 145-156.
[23]	WANG Shao-wa, GONG Dao-yi, 2000. Enhancement of the warming trend in China [J]. Geophysical Research Letters, 27 (16): 2581-2584.
[24]	WU Xiang-ding, LIN Zhen-yao, 1981. Climatic change during the last 2000 years in Tibet [A]. In: Proceedings of Symposium on Climatic Change [C]. Beijing: Science Press, 18-25. (in Chinese)
[25]	YAO Tan-dong, THOMPSON L G, QIN Da-he et al., 1996.Variations in temperature and precipitation in the past 2000 a on the Xizang (Tibet) Plateau-Guliya ice core record [J].Science in China (Series D), 39 (4) : 459-467.
[26]	ZHANG De-er, 1994. Evidence for the existence of the Medieval Warm Period in China [J]. Climate Change, 3: 289-297.
[27]	ZHANG Pei-yuan, 1996. Climate Change in China during Historical Times [M]. Jinan: Scientific and Technological Press, 435-436. (in Chinese)
[28]	ZHU Ke-zhen, 1973. A preliminary study on the climatic fluctuations during the last 5 000 years in China [J]. Scientia Sinica, 16: 226 -256.

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通讯作者: 陈斌, bchen63@163.com

1.
沈阳化工大学材料科学与工程学院沈阳 110142

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CLIMATIC VARIATIONS IN CHINA OVER THE LAST 2000 YEARS

1. Cold and And Regions Environmental and Engineering Research Institute, the Chinese Academy of Sciences, Lanzhou 730000, P. R. China;

2. Institute of Geography and Limnology, the Chinese Academy of Sciences, Nanjing 210008, P. R. China

Funds: Under the auspices of the KZCX2-304 and KI 951-A1-202-04 Project of the Chinese Academy of Sciences.

Received Date: 2001-02-13

Publish Date: 2001-06-20

Key words:

Abstract: A compilation of paleoclimate records from ice core, tree-rings, lake sediments and historical documents provides a view of temperature change in China over the recent 2000 years. For all-China temperature reconstruction, six sub-stages are identified for the last two millennia. Around AD 0-240, AD 800-1100, AD 1320-1400 and the period from AD 1880 on were warm while around AD 240-800, AD 1100-1320, AD 1400-1880 were cold. Also, temperature varied from region to region in each of the warm or cold periods. The Eastern Han warm period (0-AD 240), the cold period covering the span of Wei, Jin, and the Southern and Northern Dynasties, the MWP (AD 800-1100) and succeeding LIA occurred in eastern China and the Qilian Mountains. Only the fint two climatic events were recorded in Guliya ice core while the so-called MWP and LIA was far weaker. Also, the warming between AD 800 and 1100 didn't occur in the south of Xizang (Tibet) Plateau. Instead, the southern Xizang Plateau experienced warming in AD 1150-1400. The aggregated China temperature agrees well with North-hemisphere temperature in the past millennia, indicating close relationship of temperature changes between China and North-hemisphere.

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Reference (28)

[1]	BRADLEY R S,. JONES P D, 1993. 'Little Ice Age' summer temperature variations: their nature and relevance to recent global warming trends [J]. The Holocene, 3: 367-376.
[2]	BRAEUNING A, 1999. Zur Dendroklimatologie Hochtibets wahrend desletzten Jahrtausends [C]. Dissertationes Botanicae.
[3]	BRIFFA K R, 2000. Annual climate variability in the Holocene: interpreting the message of ancient trees [J]. Quaternary Science Reviews, 19: 87-105.
[4]	CROWLEY T J, LOWERY T S, 2000. How warm was the Medieval .Warm Period [J]. Ambio, 29(1): 51-54.
[5]	FUKUSAWA H, 1995. High-resolution reconstruction of environmental changes from the last 2000 years varied sediments in Lake Suigetsu central Japan [A]. In: Paleoclimate and Environmental Variability in AustraGAsianTransect during the Past 2000 Years [C], (Proceedings of the 1995 Nagoya IGBP-PAGES/PEP-Ⅱ Symposium) Nagoya University. Nagoya, Japan,84-89.
[6]	HONG Ye-tang, JIANG Hong-bo et al., 2000. Response of climate to solar forcing recorded in a 6000-year δ¹⁸O time-series of Chinese peat cellulose [J]. The Holocene, 10 (1): 1-7.
[7]	HUGHES M K, DIAZ H F, 1994. Was there a 'Medieval Warm Period', and if so, where and when [J]. Climatic Change, 26(2): 109-142.
[8]	INOUCHI Y, YOKOTA S, TERASHIMA S, 1995. Climatic changes around Lake Biwa during the past 300 000 years anc 2000 years [A]. In: Paleoclimate and Environmental variability in Austral-Asian Transect during the Past 2000 Yean [C] (Proceedings of the 1995 Nagoya IGBP-PAGES/PEP-Ⅱ Symposium). Nagoya University, Nagoya, Japan, 109-114.
[9]	JONES P D, BRADLEY R S, 1992. Climatic variations over thc last 500 years [A]. In: BRADLEY R S, JONES P 1: (eds.). Climate since A. D. 1500 [C]. London: Routledge, 649-665.
[10]	JONES P D, BRIFFA K R, Barnett T P et al., 1998.High-resolution palaeoclimatic records for the last millennium:Interpretation, integration and comparison with General Circulation Model control-run temperatures [J]. The Holocene, 8: 455-471.
[11]	JONES P D, OSBORN T J, BRIFFA K R, 1999. Estimatinl sampling errors in larger-scale temperature averages [J].Journal of Climate, 10: 2548-2568.
[12]	KANG Xing-cheng, GRAUMLICH L J, SHEPPARD P R, 1997.The last 1835 years climate changes inferred from tree rinl records in Dulan region, Qinghai, China [JI . Quaternar:Sciences, 1 : 70-75.
[13]	KITAGAWA H, 1995. Climatic implications in a Japanese ceda (Crhptomeria Japonica) during the last two millennia [J].Geophys. Res. Lett., 22(16): 2155 -2188.
[14]	LAMB H H, 1965. The early Medieval Warm Epoch and its se. quel [J]. Palaeogeography, Palaeoclimatology, Palaeoe cology, 1: 13 -37.
[15]	LIN Xue-chun, Yu Shu-qiu, TANG Guo-li, 1995. Series of av. erage air temperature over China for the last 100-year period [J].Scientia Atmspherica Sinica, 19(5): 525 -534. (in Chinese)
[16]	Lou Jian-yu, CHEN Zheng-dong, WANN J K, 1997. Paleocli. matological records of Great Ghost Lake in Taiwan [J]. Sci. . ence in China (Series D), 40(3): 284-292.
[17]	Lou Jian-yu, CHEN Zheng-dong, 1997. Paleoclimatological an(paleoenvironmental records since 4000 a B. P. in the sedi. ments of alpine lakes in Taiwan [J]. Science in China (Serie D), 40(4): 424 -431. hANN M E, BRADLEY R S, HUGHES M K, 1999. Northern hemisphere temperatures during the past millennium: 'Inferences, uncertainties, and limitations [J]. Geophys. Res.Lett., 26: 759-762.
[18]	IVERPECK J, HUGHEN K, HARDY D, et al., 1997. Arctic environmental changes of the last four centuries [J]. Nature, 278(5341): 1251-1256.
[19]	AKAGUCHI Y, 1983. Warm and cold stages in the past 7600 years in Japan and their global correlation-Especially on climatic to the global sea level changes and the ancient Japanese history [J]. Bulletin of Department of Geography,University of Tokyo, 15: 1-31.
[20]	SHI Ya-feng, YAO Tan-dong, YANG Bao, 1999. Decadal' climatic variations recorded in Guliya ice core and comparison with the historical documentary data from East China during the last 2000 years [J]. Science in China (Series D), 42 (Supplement): 91-100.
[21]	ANG Lin-yu, SHEN Cai-ming, LIU Kam-biu et al., 2000.Changes in south Asian monsoon: New high-resolution paleoclimatic records from Tibet, China [J]. Chinese Science Bulletin, 1: 87-91.
[22]	HOMPSON L G, MOSLEY-THOMPSON E, DAVIS M E et al., 1993. Recent Warming: Ice core evidence from tropical ice cores with emphasis on Central Asia [J]. Global Planet.Change, 7: 145-156.
[23]	WANG Shao-wa, GONG Dao-yi, 2000. Enhancement of the warming trend in China [J]. Geophysical Research Letters, 27 (16): 2581-2584.
[24]	WU Xiang-ding, LIN Zhen-yao, 1981. Climatic change during the last 2000 years in Tibet [A]. In: Proceedings of Symposium on Climatic Change [C]. Beijing: Science Press, 18-25. (in Chinese)
[25]	YAO Tan-dong, THOMPSON L G, QIN Da-he et al., 1996.Variations in temperature and precipitation in the past 2000 a on the Xizang (Tibet) Plateau-Guliya ice core record [J].Science in China (Series D), 39 (4) : 459-467.
[26]	ZHANG De-er, 1994. Evidence for the existence of the Medieval Warm Period in China [J]. Climate Change, 3: 289-297.
[27]	ZHANG Pei-yuan, 1996. Climate Change in China during Historical Times [M]. Jinan: Scientific and Technological Press, 435-436. (in Chinese)
[28]	ZHU Ke-zhen, 1973. A preliminary study on the climatic fluctuations during the last 5 000 years in China [J]. Scientia Sinica, 16: 226 -256.

CLIMATIC VARIATIONS IN CHINA OVER THE LAST 2000 YEARS

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References

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通讯作者: 陈斌, bchen63@163.com

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