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《中国科学A辑(英文版)》 1973-02
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CHU KO-CHEN (CO-CHING CHU) (Academia Sinica)  
The world climate during the historical times fluctuated. The numerous Chinese historical writings provide us excellent references in studying the ancient climate of China. The present author testifies, by the materials got from the histories and excavations, that during Yin-Hsu at Anyang, the ammal temperature was about 2℃ higher than that of the, present in most of the time. After that came a series of up and down swings of 2—3℃ with minimum temperatures occurring at approximately 100 B. C. (about the end of the Yin Dynasty and the beginning of the Chou Dynasty), 400 A. D. (the Six Dynasties), 1200 A. D. (the South Snug Dynasty), and 1700 A. D. (abont the end of the Ming Dynasty and the beginning of the Ching Dynasty). In the Han and the Tang Dynasties (200 B. C.—220 A. D. and 600—900 A. D.) the climate was rather warm. When the world climate turned colder than usual, it tended to begin at the Pacific coast of Eastern Asia, propagating as a wave westward, through Japan and China, to the Atlantic coast of Europe and Africa. When the world temperature recovered, it tended to propagate eastward from the west. A fuller knowledge of lhe climatic fluctuations in historical times and a good grasp of their laws would render better service to the long-range forecasting in climate.
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Chinese Journal Full-text Database 10 Hits
1 WANG Yong1,2,3, SHEN Ji1*, XU Xingna1,4, LIU Xingqi1, SIROCKO Frank3, ZHANG Enlou1, and JI Junfeng5 1 State Key Laboratory of Lake Science and Environment, Nanjing Institute of Geography and Limnology, Nanjing 210008, China 2 Max Planck Institute of Chemistry, Mainz 55020, Germany 3 Institute of Geoscience, University of Mainz, Mainz 55099, Germany 4 School of Geographical Science, Southwest University, Chongqing 400715, China 5 Department of Earth Sciences, Nanjing University, Nanjing 210093, China;Environmental changes during the past 13500 cal. a BP deduced from lacustrine sediment records of Lake Qinghai, China[J];中国地球化学学报(英文版);2011-04
2 GE Quansheng~1 WANG Shaowu~2 WEN Xinyu~2 Caiming SHEN~3 HAO Zhixin~(*1) 1 Institute of Geographical Sciences and Natural Resources Research,Chinese Academy of Sciences,Beijing 100101 2 Department of Atmospheric Science,School of Physics,Peking University,Beijing 100871 3 Atmospheric Sciences Research Center,State University of New York,Albany,New York 12203,USA;Temperature and Precipitation Changes in China During the Holocene[J];大气科学进展(英文版);2007-06
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5 LI DongLing 1,JIANG Hui 1,LI TieGang 2 & ZHAO MeiXun 3 1 Key Laboratory of Geographic Information Science,East China Normal University,Shanghai 200062,China;2 Key Laboratory of Marine Geology and Environment,Institute of Oceanology,Chinese Academy of Sciences,Qingdao 266071,China;3 Key Laboratory of Theoretical and Applied Marine Chemistry and Chemical Engineering of the Ministry of Education,Ocean University of China,Qingdao 266100,China;Late Holocene paleoenvironmental changes in the southern Okinawa Trough inferred from a diatom record[J];科学通报(英文版);2011-11
6 XUE Chun-ting~(1,2) (1. The Key Laboratory of Marine Hydrocarbon Resources and Environmental Geology , Ministry of Land and Resources , Qingdao 266071, China; 2. Qingdao Institute of Marine Geology , Qingdao 266071, China);Origin of Coastal Landforms From the Zhangweixin River Mouth to the Tuhai River Mouth Along the West Coast of the Bohai Sea[J];Advances in Marine Science;2011-03
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8 LIU Shengfa 1,2,SHI Xuefa 1,2 ,LIU Yanguang 1,2,WU Yonghua 1,2,YANG Gang 1,2 1 First Institute of Oceanography,State Oceanic Administration,Qingdao 266061,China 2 Key Laboratory of Marine Sedimentology and Environmental Geology,State Oceanic Administration,Qingdao 266061,China;Environmental record from the mud area on the inner continental shelf of the East China Sea since the mid-Holocene[J];海洋学报(英文版);2011-04
9 YANG Bao1, SHI Ya-feng2, LI Heng-peng2 (1. Cold and Arid 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;CLIMATIC VARIATIONS IN CHINA OVER THE LAST 2000 YEARS[J];中国地理科学(英文版);2001-02
10 WU Li1,2,WANG Xinyuan2,3,ZHOU Kunshu4,MO Duowen5,ZHU Cheng1,GAO Chao2,ZHANG Guangsheng6,LI Lan1,LIU Li2,HAN Weiguang2 1.School of Geographic and Oceanographic Sciences,Nanjing University,Nanjing 210093,China;2.College of Territorial Resources and Tourism,Anhui Normal University,Wuhu 241000,Anhui,China;3.Center for Earth Observation and Digital Earth,CAS,Beijing 100190,China;4.Institute of Geology and Geophysics,CAS,Beijing 100029,China;5.College of Urban and Environmental Sciences,Peking University,Beijing 100871,China;6.Department of Urban Construction and Environment Science,West Anhui University,Lu' an 237012,Anhui,China;Transmutation of ancient settlements and environmental changes between 6000-2000 aBP in the Chaohu Lake Basin,East China[J];地理学报(英文版);2010-05
China Proceedings of conference Full-text Database 1 Hits
1 Ming Tan and Tungsheng Liu Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing,China State Key Laboratory of Loess and Quaternary Geology,Institute of Earth Environment,Chinese Academy of Sciences, Shaanxi,China Juzhi Hou and Xiaoguang Qin Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing,China Hucai Zhang Department of Geographical Sciences,Lanzhou University,Lanzhou,China Tieying Li Beijing Geological Survey Institute,Beijing.China;Cyclic rapid warming on centennial-scale revealed by a 2650-year stalagmite record of warm season temperature[A];[C];2003
Chinese Journal Full-text Database 10 Hits
1 ZHUANG Hua-feng(College of Society, Anhui Normal University, Wuhu 241000, China);THE DEVELOPMENT OF POLEDERS IN THE LOWER REACHES OF YANGTZI RIVER AND THEIR INFLUENCE ON THE ECOLOGICAL ENVIRONMENT[J];Journal of Anhui Normal University(Natural Science);2004-01
2 WANG Xin-yuan~(1,2),HE Hui,QIAN Yu-chun~3,LU Ying-cheng~1,GAO Chao~1(1.Work Station of RS Archaeology of Anhui Province,Anhui Normal Unversity, Wuhu 241000, China;2.Dept. of Earth and Space Sciences, University of science and Technology of China, Hefei 230026,China; 3.Adiminstration Place of Culture Relic of Chaohu City Chaohu 238000, China);A INFERENCE OF ANCIENT JUCHAO CITY BASED ON ENVIRONMENT ARCHAEOLOGY[J];Journal of Anhui Normal University(Natural Science);2005-01
3 Chen Jiyang (Lanzhou Institute of Glaciology and Geocryology, Chinese Academy of Sciences);Preliminary Research on the Mid-and Late-Holocene Glacial Fluctuations in Tianger Peak Ⅱ Regions, Tianshan Mountains[J];Journal of Glaciology and Geocryology;1987-04
4 JIAO Ke-qin, YAO Tan-dong, LI Shi-jie (Cold and Arid Regions Environmental and Engineering Research Institute, CAS, Lanzhou Gansu 730000 China) (Nanjing Institute of Geography and Limnology, CAS, Nanjing Jiangsu 210008. China);Evolution of Glaciers and Environment in the West Kunlun Mountains During the Past 32 ka[J];JOURNAL OF GLACIOLGY AND GEOCRYOLOGY;2000-03
5 LI Yong-hua, YIN Huai-ning, ZHANG Xiao-yong, CHEN Zhan-jiao (Urban and Environment Sciences Institute of Liaoning Normal University, Dalian Liaoning 116029, China)=;The Environment Disaster Events and the Evolution of Man-land Relation in the West Liaoning During 5 000 a BP[J];Journal of Glaciology and Geocryology;2003-01
6 CUI Jian-xin~1, ZHOU Shang-zhe~2, CHANG Hong~3(1.Research Center for the Historical Environment and the Economic Society in the Northwest,Shaanxi Normal University,Xi′an Shaanxi 710062,China;2.Department of Geography,South China Normal University,Guangzhou Guangdong510631,China;3.State Key Laboratory of Loess and Quaternary Geology,Institute of Earth Environment,Chinese Academy of Sciences,Xi'an Shaanxi 710075,China);Advances of the Geoarcheology in the Holocene[J];Journal of Glaciology and Geocryology;2005-06
7 LI Zhong-qin,SHEN Yong-ping,WANG Fei-teng,LI Hui-lin,DONG Zhi-wen,WANG Wen-bin,WANG Lin(State Key Laboratory of Cryosphere Science/Tianshan Glaciological Station,CAREERI,CAS,Lanzhou Gansu 730000,China);Response of Glacier Melting to Climate Change——Take rümqi Glacier No.1 as an Example[J];Journal of Glaciology and Geocryology;2007-03
8 HAN Tian-ding,GAO Ming-jie,YE Bai-sheng,JIAO Ke-qin(State Key Laboratory of Gryospheric Sciences,Cold and Arid Regions Environmental and Engineering Research Institute,Chinese Academy of Sciences,Lanzhou Gansu 730000,China);Characteristic of Runoff Process of the Glacier and Permaforst in the Headwaters of the rümqi River[J];Journal of Glaciology and Geocryology;2010-03
9 Lu Qianrong Wang Xiaojing ( Institute of Estuarine and Coastal Research, East China Normal University, Shanghai );CLAY MINERALS IN FINE-GRAINED SEDIMENTS AT CHANGJIANG ESTUARY AND THEIR GEOCHEMICAL CHARACTERISTICS[J];Acta Sedimentologica Sinica;1985-04
10 GUO Zhi gang YANG Zuo sheng QU Yan hui FAN De jiang(College of Marine Geosciences, Ocean University of Qingdao, Qingdao Shandong 266003);Study on Comparison Sedimentary Geochemistry of Mud Area on East China Sea Continental Shelf[J];ACTA SEDIMENTOLOGICA SINICA;2000-02
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Chinese Journal Full-text Database 10 Hits
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2 ZHANG Xin-rong1,2 HU Ke3 FANG Shi1 WANG Dong-po1 ZHENG Hongbo2(1. College of Earth Sciences, Jilin University, Changchun 130061; 2. State Key Laboratory of Marine Geology Tongji University, Shanghai 200092;3. College of Oceanography, China University of Geosciences, Beijing 100083);Construction and Application of Phyolith-climate Transfer Function in Peat Surface Deposits of Northeast China[J];Acta Sedimentologica Sinica;2008-04
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10 KUANG XueYuan1,2, LIU Jian1↑, WANG HongLi1 & WANG SuMin1 1 State Key Laboratory of Lake Science and Environment, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing 210008, China; 2 Guangxi Climate Center, Nanning 530022, China;Inter-hemispheric comparison of climate change in the last millennium based on the ECHO-G simulation[J];科学通报(英文版);2008-17
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