Original Articles

Characteristics of Holocene Temperature Change in China

Expand
  • 1. School of Life and Geographic Science, Qinghai Normal University, Xining 810008, China;
    2. School of Geography, Beijing Normal University, Beijing 100875, China

Received date: 2010-10-01

  Revised date: 2011-01-01

  Online published: 2011-09-25

Abstract

Based on the researches on temperature change in China in the Holocene, the characteristics of temperature variability were displayed in this report. The temperature variation in the Holocene could be divided into three stages: ascending in the early Holocene with great fluctuations, Megathermal in the mid-Holocene, and descending in the late Holocene. The temperature in the warmest period of 8.0-6.2 kaBP was 1℃ higher than at present. Ten cold intervals which occurred in 11.0 kaBP, 9.8 kaBP, 9.2 kaBP, 8.9 kaBP, 8.2 kaBP, 6.2 kaBP, 4.0 kaBP, 2.8 kaBP, 1.5 kaBP and 0.4 kaBP were consistent with the eight cold events in the North Atlantic domain. It seems that the most significant cold-events appeared in 4.0 kaBP and 0.4 kaBP. Warm events occurred around 8.6 kaBP, 4.7 kaBP and 3.5 kaBP. The significant periodicities of temperature variation in the Holocene were 1000a and 700a.

Cite this article

HOU Guangliang, FANG Xiuqi . Characteristics of Holocene Temperature Change in China[J]. PROGRESS IN GEOGRAPHY, 2011 , 30(9) : 1075 -1080 . DOI: 10.11820/dlkxjz.2011.09.001

References

[1] Mackay A, Battarbee R, Oldfield F. Global change in theholocene. Oxford: Oxford University Press, 2005:227-241.

[2] PAGES. PAGES (2009) Science Plan and ImplementationStrategy.IGBP Report No. 57. IGBP Secretariat,2009, Stockholm: 1-67.

[3] Hafstan U. A subdivision of the late Pleistocene period ona synchronous basis intended fro global and universal usage.Pleogeography, Paleoclimatology and Paleoecology,1976, 7: 279-296.

[4] Stuiver M, Braziunas T F, Grootes P M, et al. Is there evidencefor solar forcing of climate in the GISP2 oxygenisotope record. Quaternary Research, 1997, 48: 259-266.

[5] Anderson D E, Goudie A S,Parker A G. Global Environmentsthrough the Quaternary. Oxford: Oxford UniversityPress, 2007.

[6] Bond G, Showers W, Cheseby M, et al. A pervasive millennial-scale cycle in North Atlantic Holocene and glacialclimates, Science, 1997, 278(21): 1257-1263.

[7] Rasmussen S O, Vinther B M, Clausen H B, et al. EarlyHolocene climate oscillations recorded in three Greenlandice cores. Quaternary Science Reviews, 2007, 26(3):1907-1914.

[8] Sirocko F, Garbe-Schonberg D, McIntyre A, et al. Teleconnectionsbetween the subtropical monsoon andhigh-latitudem climates during the last deglaciation. Science,1996, 272(26): 526-529.

[9] Steinhilber F, Beer J, Franlich C. Total solar irradianceduring the Holocene. Geophys. Geophysical ResearchLetters, 2009, 36, L19704, doi: 10.1029/2009GL040142.

[10] 竺可桢. 中国近五千年来气候变迁的初步研究. 中国科学, 1973(2): 168-189.

[11] 中国科学院贵阳地球化学研究所第四纪孢粉组、14C组. 辽宁省南部一万年来自然环境的演变. 中国科学,1977(6): 604-614.

[12] 施雅风.中国全新世大暖期气候与环境.北京: 海洋出版社, 1992.

[13] 张丕远.中国历史时期气候变化. 济南: 山东科学技术出版社, 1996.

[14] 唐领余, 沈才明, 赵希涛, 等. 江苏建湖庆丰剖面1 万年来的植被与气候. 中国科学: B辑, 1993, 23(6): 637-643.

[15] 宋长青, 吕厚远, 孙湘君. 中国北方花粉-气候因子转换函数建立及应用. 科学通报, 1997, 42(20): 2182- 2185.

[16] 张兰生, 方修琦, 任国玉. 我国北方农牧交错区的环境演变. 地学前缘,1997, 4(1-2): 127-134.

[17] 唐领余, 沈才明, 廖淦标, 等. 末次盛冰期以来西藏东南部的气候变化: 西藏东南部的花粉记录. 中国科学: D辑, 2004, 34 (5): 436-442.

[18] 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. 科学通报, 2001,46(12): 1040-1044.

[19] 刘嘉麒, 吕厚远, Negendank J, 等. 湖光岩玛珥湖全新世气候波动的周期性. 科学通报, 2000, 45(11): 1190-1195.

[20] 王绍武, 龚道溢. 全新世几个特征时期中国气温. 自然科学进展, 2000, 10(4): 325-332.

[21] 葛全胜, 王顺兵, 郑景云. 过去5000 年中国气温变化序列的重建. 自然科学进展, 2006, 16(6): 689-696.

[22] 方修琦,侯光良. 中国全新世气温序列的集成重建. 地理科学, 2011, 31(4): 385-393.

[23] 王绍武. 全新世北大西洋冷事件: 年代学和气候影响.第四纪研究, 2009, 29(6): 1146-1153.

[24] 黄嘉佑. 气象统计分析与预报方法. 北京: 气象出版社,2000: 19-28.

[25] Rapp D. Assessing climate change. Chichester: PraxisPress, 2008: 32-39.

[26] Ge Q S, Zheng J Y, Fang X Q, et al.Temperature changesof winter-half-year in eastern China during the past 2000years. The Holocene, 2003, 13(6): 933-940.

[27] Bond G, Kromer B, Beer J, et al. Persistent solar influenceon north atlantic climate change during holocene.Science, 2001, 294(13): 2130-2135.

[28] 黄元辉, 黄玥, 蒋辉. 南海北部15 kaBP 以来表层海水温度变化: 来自海洋硅藻的记录. 海洋地质与第四纪地质,2007, 27(5): 65-73.

[29] 朱诚, 马春梅, 张文卿, 等. 神农架大九湖15.753kaBP.以来的孢粉记录和环境演变. 第四纪研究, 2006, 26(5):814-826.

[30] 程波, 陈发虎, 张家武. 共和盆地末次冰消期以来的植被和环境演变. 地理学报, 2010, 65(11): 1336-1344.

[31] 靳鹤龄, 董光荣, 苏志珠, 等. 全新世沙漠-黄土边界带空间格局的重建. 科学通报, 2001, 46(7): 538-543.

[32] 李容全. 中国北方冰缘与分期. 第四纪研究, 1990, 10(2):125-136.

[33] 于学峰, 周卫健, Franzen L G, 等. 青藏高原东部全新世冬夏季风变化的高分辨率泥炭记录. 中国科学: D 辑,2006, 36(2): 182-187.

[34] 王绍武. 4.2kaBP 事件. 气候变化研究进展, 2009, 5(3):142-144.

[35] 邵晓华, 汪永进, 程海, 等. 全新世季风气候演化与干旱事件的湖北神农架石笋记录. 科学通报, 2006, 51(1):80-86.

[36] Dykoski C A,Edwards R L, Cheng H, et al. A high-resolution,absolute-dated Holocene and deglacial asian monsoonrecord from Dongge cave. Chin. Earth and PlanetaryScience Letters, 2005, 233(6): 71-86.

[37] 吴文祥, 刘东生. 4000 a BP前后东亚季风变迁与中原周围地区新石器文化的衰落. 第四纪研究, 2004, 24(3):278-284.

[38] 邓辉. 全新世大暖期盐北地区人地关系的演变. 地理学报, 1997, 52(1): 64-71.

[39] 方修琦, 孙宁. 降温事件: 4.3kaBP 岱海老虎山文化中断的可能原因. 人文地理, 1998, 13(1): 71-76.

[40] 侯光良, 刘峰贵, 刘翠华, 等. 中全新世甘青地区古文化变迁的环境驱动. 地理学报, 2009, 64(1): 53-58.

[41] 高华中, 朱诚, 曹光杰. 山东沂沭河流域2000BC前后古文化兴衰的环境考古. 地理学报,2006, 61(3): 255-261.

[42] 史威, 马春梅, 朱诚, 等. 太湖地区多剖面地层学分析与良渚期环境事件. 地理研究,2008, 27(5): 1129-1138.

[43] 王绍武, 叶瑾琳, 龚道溢. 中国小冰期的气候. 第四纪研究, 1998, 18(1): 54-64.

[44] Chen Fa hu, Zhu Yan, Li Jijun, et al. Abrupt Holocenechanges of the Asian monsoon at millennial and centennialscales. Chinese Science Bulletin, 2001, 46(23):1942-1947.

[45] 靳立亚, 陈发虎, 朱艳. 西北干旱区湖泊沉积记录反映的全新世气候波动周期性变化. 海洋地质与第四纪地质, 2004, 24(2): 101-108.

[46] Feng S, 夏敦胜, 汤懋苍, 等. 秦安地区全新世气候的周期振荡特征. 冰川冻土, 2006, 28(1): 70-75.

[47] 方修琦, 葛全胜, 郑景云. 全新世寒冷事件与气候变化的千年周期. 自然科学进展, 2004, 14(4): 456-461.
Outlines

/