中国西北干旱区小冰期的湿度变化特征

doi:10.11821/xb200801003

地理学报 ›› 2008, Vol. 63 ›› Issue (1): 23-33.doi: 10.11821/xb200801003

中国西北干旱区小冰期的湿度变化特征

陈建徽¹, 陈发虎¹, 张家武¹, 杨保²

1. 兰州大学西部环境教育部重点实验室, 兰州730000;
2. 中国科学院寒区旱区环境与工程研究所, 兰州730000

收稿日期:2007-09-20 修回日期:2007-10-23 出版日期:2008-01-25 发布日期:2008-01-25
通讯作者: 陈发虎(1962-), 男, 教授, 中国地理学会常务理事. 主要从事环境变化研究。E-mail: fhchen@lzu.edu.cn
作者简介:陈建徽(1981-), 男, 博士研究生, 主要从事气候变化与湖泊生态研究。E-mail: chenjianhui.lzu@hotmail.com
基金资助:
国家自然科学基金重点项目(90502008); 国家自然科学基金创新研究群体科学基金项目(40421101) 联合资助

Humidity Variability in the Arid Northwest China during LIA Derived from Different Proxy Records

CHEN Jianhui¹, CHEN Fahu¹, ZHANG Jiawu¹, YANG Bao²

1. MOE Key Laboratory of West China's Environmental System, Lanzhou University, Lanzhou 730000, China;
2. Cold and Arid Regions Environmental and Engineering Research Institute, CAS, Lanzhou 730000, China

Received:2007-09-20 Revised:2007-10-23 Online:2008-01-25 Published:2008-01-25
Supported by:
Key Project for National Natural Science Foundation of China, No.90502008; Innovation Team Project for National Natural Science Foundation of China, No.40421101

摘要/Abstract

摘要：

选取中国西北干旱区11 条具有明确古湿度指示意义的气候记录, 结合冰芯、地层沉积、湖泊沉积、树木年轮、河流阶地等各种研究资料和历史记载, 研究中国西北干旱区小冰期的湿度变化。结果表明研究区小冰期(1400-1920 AD) 从整体而言处于相对湿润的阶段: 区内高大山系降水处于较高时段— —西昆仑山古里雅冰芯积累量增大, 天山山间湖泊水位回升, 祁连山敦德冰芯孢粉总浓度增加; 而盆地内流系统水量也出现了相应的变化— —塔里木盆地克里雅河和塔里木河流量增大, 准噶尔盆地艾比湖水位上升, 巴丹吉林沙漠地下水补给量上升, 居延海入湖水量增大, 湖面扩展, 青海湖盆地降水增加, 有效湿度增大, 苏干湖水体盐度降低, 入湖水量/ 蒸发量之比升高。同时, 较高分辨率的湿度资料显示, 研究区东—南边缘地带在小冰期内部存在次一级的干湿波动, 两个湿度较高的时期出现在16 世纪和18 世纪, 分别与小冰期内部的两个相对温暖时期有很好的对应。中国西北相对湿润的小冰期主要是西风带强度增加和位置南移造成该区域降水增多和全球性普遍降温导致有效湿度增大两个因素共同作用的结果, 研究区边缘地带小冰期内部冷干暖湿的配置则主要体现了夏季风的影响。

关键词: 小冰期, 中国西北干旱区, 湿度

Abstract:

Eleven major humidity proxy records and other supplementary evidences including different natural archives such as ice-cores, sedimentary records, river terraces, lake-level fluctuations as well as historical documents are involved to reconstruct the humidity variability in the arid Northwest China during the Little Ice Age (LIA) from 1400 AD to 1920 AD. The result shows that as a whole, the LIA is a relatively humid period in this region, contrasting to last 100 years during global warming and medieval warming period. For instance, precipitation in high marginal mountains of the study area was of a high value reflected by the various proxy records from west Kunlun, Tianshan and Qilian mountains. Accordingly, the discharge of big endorheic rivers such as the Tarim and Keliya rivers increased; the surface areas of terminal lakes in desert field expanded, e.g., at Juyan Lake and Ebinur Lake; the water levels rose at lakes in intermontane basins, such as Bosten Lake, Balikun Lake and Qinghai Lake; the groundwater recharge rates in the Badain Jaran Desert were increased; and the water salinity of Sugan Lake also significantly decreased during the LIA. Furthermore, the humidity records with a relatively high resolution from the eastern-southern fringe of the arid Northwest China indicate that there is a secondary oscillation of wet and dry within the LIA. The relatively high humidity during the LIA in Northeast China possibly results from the increase of precipitation in this region due to the strengthening and southward shift of westerlies and the decrease of evapotranspiration caused by the cooling during that time.

Key words: arid Northwest China, Little Ice Age (LIA), humidity variability

陈建徽,陈发虎,张家武,杨保. 中国西北干旱区小冰期的湿度变化特征[J]. 地理学报, 2008, 63(1): 23-33.

CHEN Jianhui,CHEN Fahu,ZHANG Jiawu,YANG Bao. Humidity Variability in the Arid Northwest China during LIA Derived from Different Proxy Records[J]. Acta Geographica Sinica, 2008, 63(1): 23-33.

参考文献

[1] Bradley R S, Jones P D. Climate since A.D. 1500. London: Routledge, 1992. 649-655.

[2] Wang Shaowu, Ye Jinlin, Gong Daoyi. Climate in China during Little Ice Age. Quaternary Sciences, 1998, 18(1): 54-62.
[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): 54-62.]

[3] Grove J M. The initiation of the "Little Ice Age" in regions around the North Atlantic. Climatic Change, 2001, 48: 53-82.

[4] Landsberg H E. Historic weather data and early meteorological observations. In: Hecht A D (ed.). Palaeoclimatic Analysis and Modelling. New York: Wiley, 1985. 27-69.

[5] Ogilvie A E J, Jónsson T. "Little Ice Age" Research: A perspective from Iceland. Climatic Change, 2001, 48: 9-52.

[6] Jones P D, Briffa K R, Barnett T P et al. High-resolution palaeoclimatic records for the last millennium: Interpretation, integration and comparison with General Circulation Model control-run temperatures. Holocene, 1998, 8(4): 455-471.

[7] Mann M E, Bradley R S, Hughes M K. Northern Hemisphere temperatures during the past millennium: Inferences, uncertainties, and limitations. Geophysical Research Letters, 1999, 26(6): 759-762.

[8] Jones P D, Osborn T J, Briffa K R. The evolution of climate over the last millennium. Science, 2001, 292: 662-667.

[9] Morberg A, Sonechkin D M, Holmgren K et al. Highly variable Northern Hemisphere temperatures reconstructed from low- and high-resolution proxy data. Nature, 2005, 433: 613-617.

[10] Osborn T J, Briffa K R. The spatial extent of 20th-century warmth in the context of the past 1200 years. Science, 2006, 311: 841-844.

[11] Soon W, Baliunas S. Proxy climatic and environmental changes of the past 1000 years. Climate Research, 2003, 23: 89-110.

[12] Grove J M. The onset of the Little Ice Age. In: Jones P D, Ogilvie A E J, Davies T D et al. (eds). History and Climate: Memories of the Future? New York: Kluwer Academic Publishers, 2001. 153-185.

[13] Jones P D, Briffa K R. The "Little Ice Age": Local and global perspectives. Climatic Change, 2001, 48: 5-8.

[14] Wang Shaowu, Wang Risheng. Little Ice Age in China. Chinese Science Bulletin, 1991, 36(3): 217-220.
[王绍武, 王日昇. 中国的小冰河期. 科学通报, 1990, 35(10): 769-772.]

[15] Zhang De'er. The Little Ice Age in China and its correlations with global change. Quaternary Sciences, 1991, 11(2): 104-111.
[张德二. 中国的小冰期气候及其与全球变化的关系. 第四纪研究, 1991, 11(2): 104-111.]

[16] Wang Sumin, Liu Jian, Zhou Jing. The climate of Little Ice Age Maximum in China. Journal of Lake Sciences, 2003, 15(4): 369-376.
[王苏民, 刘健, 周静. 我国小冰期盛期的气候环境. 湖泊科学, 2003, 15(4): 369-376.]

[17] Wang Shaowu, Wen Xinyu, Luo Yong et al. The reconstruction of temperature series in China for the last 1000 years. Chinese Science Bulletin, 2007, 52(8): 958-964.
[王绍武, 闻新宇, 罗勇等. 近千年中国温度序列的建立. 科学通报, 2007, 52(8): 958-964.]

[18] Zheng Jingyun, Wang Shaowu. Assessment on climate change in China for the last 2000 years. Acta Geographica Sinica, 2005, 60(1): 21-31.
[郑景云, 王绍武. 中国过去2000 年气候变化的评估. 地理学报, 2005, 60(1): 21-31.]

[19] Ge Q S, Zheng J Y, Fang X Q et al. Winter half-year temperature reconstruction for the middle and lower reaches of the Yellow River and Yangtze River, China, during the past 2000 years. Holocene, 2003, 13(6): 933-940.

[20] Yang B, Braeuning A, Johnson K R et al. General characteristics of temperature variation in China during the last two millennia. Geophysical Research Letters, 2002, 29(9): 10.1029/2001GL014485.

[21] Zhu Kezhen. A preliminary study on climate changes since the last 5000 years in China. Acta Archaeologica Sinica, 1972, (1): 168-189.
[竺可桢. 中国近五千年来气候变迁的初步研究. 考古学报, 1972, (1): 168-189.]

[22] Wang S W, Gong D Y, Zhu J H. 20th century climate warming in China in the context of Holocene. Holocene, 2001, 11(3): 313-321.

[23] Yao Tandong, Xie Zichu, Wu Xiaoling et al. Climatic change since Little Ice Age recorded by Dunde ice cap. Science in China (Series B), 1991, 34(6): 760-767.
[姚檀栋, 谢自楚, 武筱舲等. 敦德冰帽中的小冰期气候记录. 中国科学(B 辑), 1990, 20(11): 1196-1201.]

[24] Zhang Xiangsong, Wang Zongtai. Variability and future changes in glaciers in Northwest China. In: Shi Yafeng (ed.). Impact of Climatic Change on the Water Resources in Northwest and North China. Jinan: Shandong Science and Technology Press, 1995. 53-78.
[张祥松, 王宗太. 西北冰川变化及其趋势. 见: 施雅风主编. 气候变化对西北华北水资源的影响. 济南: 山东科学技术出版社, 1995. 53-78.]

[25] Wang Shaowu, Dong Guangrong (eds.). Environmental Characteristics and Changes in Western China. Beijing: Science Press, 2002. 43-53.
[王绍武, 董光荣主编. 中国西部环境特征及其演变. 北京: 科学出版社, 2002. 43-53.]

[26] Wang Zongtai. The Little Ice Age of Northwest China. Journal of Arid Land Resources and Environment, 1991, 5(3): 64-74.
[王宗太. 中国西北地区的小冰期. 干旱区资源与环境. 1991, 5(3): 64-74.]

[27] Ren Mei'e, Yang Renzhang, Bao Haosheng (eds.). An Outline of China's Physical Geography. Beijing: The Commercial Press, 1979. 324-337.
[任美锷, 杨纫章, 包浩生主编. 中国自然地理纲要. 北京: 商务印书馆, 1979. 324-337.]

[28] Yao Tandong, Thompson L G, Qin Dahe et al. Variations in temperature and precipitation in the past 2000a on the Xizang (Tibet) Plateau: Guliya ice core records. Science in China (Series B), 1996, 39(4): 425-433.
[姚檀栋, 秦大河, 田立德等. 青藏高原2ka 来温度与降水变化: 古里雅冰芯记录. 中国科学(D 辑), 1996, 26(4): 348-353.]

[29] Van Campo E, Cour P, Huang S X. Holocene environmental changes in Bangong Co basin (Western Tibet). Part 2: The pollen record. Palaeogeography Palaeoclimatology Palaeoecology, 1996, 120: 49-63.

[30] Zhong Wei, Xiong Heigang. Paleo-climatic and environmental development since about 4 ka B.P. and the relation with abandonments of ancient cities in southern Xinjiang. Journal of Desert Research, 1999, 19(4): 343-347.
[钟巍, 熊黑钢. 塔里木盆地南缘4ka B.P.以来气候环境演化与古城镇废弃事件关系研究. 中国沙漠, 1999, 19(4): 343-347.]

[31] Chen Fahu, Huang Xiaozhong, Zhang Jiawu et al. Humid Little Ice Age in arid central Asia documented by Bosten Lake, Xinjiang, China. Science in China (Series D), 2006, 49(12): 1280-1290.
[陈发虎, 黄小忠, 张家武等. 新疆博斯腾湖记录的亚洲内陆干旱区小冰期湿润气候研究. 中国科学(D 辑), 2007, 37(1): 77-85.]

[32] Wu Jinglu, Liu Jianjun, Wang Sumin. Climatic change record from stable isotopes in Lake Aibi, Xinjiang during the past 1500 years. Quaternary Sciences, 2004, 24(5): 585-590.
[吴敬禄, 刘建军, 王苏民. 近1500 年来新疆艾比湖同位素记录的气候环境演化特征. 第四纪研究, 2004, 24(5): 585-590.]

[33] Ma Jinzhu, Chen Fahu, Zhao Hua. Groundwater recharge and climatic change during the last 1000 years from unsaturated zone of SE Badain Jaran Desert. Chinese Science Bulletin, 2004, 48(14): 1469-1474.
[马金珠, 陈发虎, 赵华. 1000 年以来巴丹吉林沙漠地下水补给与气候变化的包气带地球化学记录. 科学通报, 2004, 49(1): 22-26.]

[34] Zhang Zhenke, Wu Ruijin, Wang Sumin et al. Environmental changes recorded by lake sediments from east Juyanhai Lake in Inner Mongolia during the past 2600 years. Journal of Lake Sciences, 1998, 10(2): 44-51.
[张振克, 吴瑞金, 王苏民等. 近2600 年来内蒙古居延海湖泊沉积记录的环境变迁. 湖泊科学, 1998, 10(2): 44-51.]

[35] Liu K B, Yao Z Y, Thompson L G. A pollen record of Holocene climatic changes from Dunde ice cap,Qinghai-Tibetan Plateau. Geology, 1998, 26(2): 135-138.

[36] Zhang Jiawu, Jin Ming, Chen Fahu et al. High-resolution precipitation variations in the Northeast Tibetan Plateau over the last 800 years documented by sediment cores of Qinghai Lake. Chinese Science Bulletin, 2003, 48(14): 1451-1456.
[张家武, 金明, 陈发虎等. 青海湖沉积岩芯记录的青藏高原东北部过去800 年以来的降水变化. 科学通报, 2004, 49(1): 10-14.]

[37] Ji J, Shen J, Balsam W et al. Asian monsoon oscillations in the northeastern Qinghai-Tibet Plateau since the late glacial as interpreted from visible reflectance of Qinghai Lake sediments. Earth and Planetary Science Letters, 2005, 233(1-2): 61-70.

[38] Shi Yafeng, Yao Tandong, Yang Bao. Decadal climatic variations recorded in Guliya ice core and comparison with the historical documentary data from East China during the last 2000 years. Science in China (Series D), 1999, 42(Supp.): 91-100.
[施雅风, 姚檀栋, 杨保. 近2000a 古里雅冰芯10a 尺度的气候变化及其与中国东部文献记录的比较. 中国科学(D 辑), 1999, 29(增刊1): 79-86.]

[39] Yao Tandong, Jiao Keqin, Yang Meixue. Precipitation variations recorded in Guliya ice core in the past 400 years. Progress in Natural Science, 2000, 10(4): 288-293.
[姚檀栋, 焦克勤, 杨梅学. 古里雅冰芯中过去400a 降水变化研究. 自然科学进展, 1999, 9(12): 1161-1165.]

[40] Shao Xuemei, Huang Lei, Liu Hongbin et al. Reconstruction of precipitation variation from tree rings in recent 1000 years in Delingha, Qinghai. Science in China (Series D), 2005, 48(7): 939-949.
[邵雪梅, 黄磊, 刘洪滨等. 树轮记录的德令哈地区千年降水变化. 中国科学(D 辑), 2004, 34(2): 145-153.]

[41] Van Campo E, Gasse F. Pollen- and diatom-inferred climatic and hydrological changes in Sumxi Co basin (Western Tibet) since 13,000 yr B.P. Quaternary Research, 1993, 39: 300-313.

[42] Liu B (ed.). Climate Changes in Southern Tarim Basin. Tokyo: Ancient and Present-Day Bookstore, 1976.

[43] Yang X P, Zhu Z D, Jaekel D et al. Late Quaternary palaeoenvironment change and landscape evolution along the Keriya River, Xinjiang, China: the relationship between high mountain glaciation and landscape evolution in foreland desert regions. Quaternary International, 2002, 97/98: 155-166.

[44] Yang X P. Geomorphological investigations in arid NW China with special attention to Badanjilin and Takelamagan. Goettinger Geographische Abhandlungen, 1991, 96: 1-124.
[Geomorphologische Untersuchungen in Trockenr!umen NW-Chinas unter besonderer Berücksichtigung von Badanjilin und Takelamagan. G"ttinger Geographische Abhandlungen, 1991, 96: 1-124.]

[45] Tian Wencheng (ed.). Bohu County Annals. Urumqi: Xinjiang University Press, 1993. 73.
[田文成主编. 博湖县志. 乌鲁木齐: 新疆大学出版社, 1993. 73.]

[46] Mahpir J, Tursunov A A (eds.). An Introduction to the Hydro-ecology in the Central Asia. Urumqi: Xinjiang Science, Technology and Hygiene Press, 1996. 149.
[加帕尔·买合皮尔, A·A·图尔苏诺夫主编. 亚洲中部湖泊水生态学概论. 乌鲁木齐: 新疆科技卫生出版社, 1996. 149.]

[47] Qin Boqiang, Shi Yafeng. Changes of inland lakes of Asia since Holocene. In: Shi Yafeng (ed.). Advances on Studies of Climate in China and Sea Level Variation. Beijing: China Ocean Press, 1992. 134-135.
[秦伯强, 施雅风. 全新世一万年来亚洲内陆湖泊的变化. 见: 施雅风主编. 中国气候与海平面变化研究进展. 北京: 海洋出版社, 1992. 134-135.]

[48] Wu Jinglu, Shen Ji, Wang Sumin et al. Characteristics of an early Holocene climate and environment from lake sediments in Ebinur region, NW China. Science in China (Series D), 2005, 35(2): 258-265.
[吴敬禄, 沈吉, 王苏民等. 新疆艾比湖地区湖泊沉积记录的早全新世气候环境特征. 中国科学(D 辑), 2003, 33(7): 569-575.]

[49] Zhang Hong, Jin Heling, Xiao Honglang et al. Soluble salt sediments of east Juyan Lake and its indicating palaeoclimate environment changes. Journal of Desert Research, 2004, 24(4): 409-415.
[张洪, 靳鹤龄, 肖洪浪等. 东居延海易溶盐沉积与古气候环境变化. 中国沙漠, 2004, 24(4): 409-415.]

[50] Fredskild B, Wagner P. Pollen and fragments of plant tissue in core samples from the Greenland ice cap. Boreas, 1974, 3: 105-108.

[51] Leng M J. Stable-isotopes in lakes and lake sediment archives. In: Mackay A, Battarbee R, Birks J et al. (eds.). Global Change in the Holocene. London: Arnold, 2003. 124-139.

[52] Henderson A C G, Holmes J A, Zhang J W et al. A carbon- and oxygen-isotope record of recent environmental change from Qinghai Lake, NE Tibetan Plateau. Chinese Science Bulletin, 2003, 48(14): 1463-1468.

[53] Chen Jing'an, Wan Guojiang, Zhang David Dian et al. Environmental records of lacustrine sediments in different time scales: Sediment grainsize as an example. Science in China (Series D), 2004, 34(10): 954-960.
[陈敬安, 万国江, 张峰等. 不同时间尺度下的湖泊沉积物环境记录: 以沉积物粒度为例. 中国科学(D 辑), 2003, 33(6): 563-568.]

[54] Nederbragt A J, Thurow J W. A 6000 yr varve record of Holocene climate in Saanich Inlet, British Columbia, from digital sediment colour analysis of ODP Leg 169s cores. Marine Geology, 2001, 174(1-4): 95-110.

[55] Grove A T. The "Little Ice Age" and its geomorphological consequences in Mediterranean Europe. Climatic Change, 2001, 48: 121-136.

[56] Ogilvie A E J, Barlow L K, Jennings A E. North Atlantic climate c. A.D. 1000: Millennial reflections on the Viking discoveries of Iceland, Greenland and North America. Weather, 2000, 55: 34-45.

[57] Holmgren K, Karlén W, Lauritzen S E et al. A 3000-year high-resolution stalagmite-based record of palaeoclimate for northeastern South Africa. Holocene, 1999, 9(3): 295-309.

[58] Petersen K L. A warm and wet little climatic optimum and a cold and dry Little Ice Age in the southern Rocky Mountains, USA. Climatic Change, 1994, 26(2/3): 243-269.

[59] Haug G H, Hughen K A, Sigman D M et al. Southward migration of the intertropical convergence zone through the Holocene. Science, 2001, 293: 1304-1308.

[60] Cioccale M A. Climatic fluctuations in the central region of Argentina in the last 1000 years. Quaternary International, 1999, 62: 35-47.

[61] Fritz S C, Ito E, Yu Z et al. Hydrologic variation in the northern Great Plains during the last two millennia. Quaternary Research, 2000, 53(2): 175-184.

[62] Li Jijun. The patterns of environmental changes since late Pleistocene in northwestern China. Quaternary Sciences, 1990, 10(4): 197-204.
[ 李吉均. 中国西北地区晚更新世以来环境变迁模式. 第四纪研究, 1990, 10(4): 197-204.]

[63] Luo Chao, Yang Dong, Peng Zicheng et al. Climatic and environmental records in the sediment of the Luobei billabong in Lop-Nur, Xinjiang in recent 32ka. Quaternary Sciences, 2007, 27(1): 114-121.
[罗超, 杨东, 彭子成等. 新疆罗布泊地区近3.2 万年沉积物的气候环境记录. 第四纪研究, 2007, 27(1): 114-121.]

[64] Shi Yafeng, Kong Zhaochen, Wang Sumin et al. Climates and environments of the Holocene megathermal maximum in China. Science in China (Series B), 1994, 37(4): 481-493.
[施雅风, 孔昭宸, 王苏民等. 中国全新世大暖期鼎盛阶段的气候与环境. 中国科学(B 辑), 1993, 23(8): 865-873.]

[65] Chen Fahu, Huang Xiaozhong, Yang Meilin et al. Westerly dominated Holocene climate model in arid central Asia: Case study on Bosten Lake, Xinjiang, China. Quaternary Sciences, 2006, 26(6): 881-887.
[ 陈发虎, 黄小忠, 杨美临等. 亚洲中部干旱区全新世气候变化的西风模式: 以新疆博斯腾湖记录为例. 第四纪研究, 2006, 26(6): 881-887.]

[66] Shi Yafeng. Glacier recession and lake shrinkage indicating a climatic warming and drying trend in central Asia. Acta Geographica Sinica, 1990, 45(1): 1-13.
[施雅风. 山地冰川和湖泊萎缩指示的亚洲中部气候干暖化趋势及未来展望. 地理学报, 1990, 45(1): 1-13.]

[67] Shi Y F, Shen Y P, Kang E S et al. Recent and future climate change in northwest China. Climatic Change, 2006, 80: 379-393.

[68] Grove J M. The century time-scale. In: Driver T S, Chapman G P (eds.). Time-scales and environmental change. London: Routledge, 1996. 39-87.

[69] Hu F S, Ito E, Brown T A et al. Pronounced climatic variations in Alaska during the last two millennia. Proceedings of the National Academy of Sciences, USA, 2001, 98: 10552-10556.

[70] Verschuren D, Laird K R, Cumming B F. Rainfall and drought in equatorial East Africa during the past 1100 years. Nature, 2000, 403: 410-413.

[71] Villalba R. Tree-ring and glacial evidence for the medieval warm epoch and the little ice age in southern South America. Climatic Change, 1994, 26: 183-197.

[72] Boomer I, Aladin N, Plotnikov I et al. The palaeolimnology of the Aral Sea: A review. Quaternary Science Reviews, 2000, 19: 1259-1278.

[73] Karpychev Y A. Variations in the Caspian sea level in the historic epoch. Water Resources, 2001, 28(1): 1-14.

[74] Zhang Q B, Cheng G D, Yao T D et al. A 2326-year tree-ring record of climate variability on the northeastern Qinghai-Tibetan Plateau. Geophysical Research Letters, 2003, 30(14): 1739-1742.

[75] Yao T D, Xie Z C, Yang Q Z. Temperature and precipitation fluctuations since 1600a provided by Dunde Ice Cap, China. In: International Symposium on Glaciers-Ocean-Atmosphere Interactions, Moscow: IAHS publ 208, 1991. 61-70.

[76] Zhang Jiacheng. Historical drought and aridification in China. In: Li Kerang (ed.). The Drought Disaster and Its Reduction Measures in China, Zhengzhou: Henan Science & Technology Publishing House, 1999. 117-136.
[ 张家诚. 中国历史时期的干旱与干旱化. 见: 李克让主编, 中国历史时期的干旱与干旱化. 郑州: 河南科学技术出版社, 1999. 117-136.]

[77] Hurrell J W, van Loon H. Decadal variations in climate associated with the North Atlantic Oscillation. Climatic Change, 1997, 36: 301-326.

[78] Xue Bin. Research on Chinese lake status data base since late Quaternary. In: Yu Ge, Xue Bin, Liu Jian et al. (eds.). Lake Records from China and the Palaeoclimate Dynamics. Beijing: China Meteorological Press, 2001. 17-83.
[ 薛滨.中国晚第四纪湖泊数据库研究. 见: 于革, 薛滨, 刘健等主编. 中国湖泊演变与古气候动力学研究. 北京: 气象出版社, 2001. 17-83.]

[79] Yu Ge, Xue Bin, Wang Sumin et al. Lake records and LGM climate in China. Chinese Science Bulletin, 2000, 45(13): 1158-1164.
[于革, 薛滨, 王苏民等. 末次盛冰期中国湖泊记录及其气候意义. 科学通报, 2000, 45(3): 250-255.]

中国西北干旱区小冰期的湿度变化特征

Humidity Variability in the Arid Northwest China during LIA Derived from Different Proxy Records

PDF (PC)

赞

可视化

被引次数

摘要/Abstract

引用本文

使用本文

参考文献

相关文章 15

Metrics

本文评价

[1]	郭泽呈, 魏伟, 石培基, 周亮, 王旭峰, 李振亚, 庞素菲, 颉斌斌. 中国西北干旱区土地沙漠化敏感性时空格局[J]. 地理学报, 2020, 75(9): 1948-1965.
[2]	郭超,蒙红卫,马玉贞,李丹丹,胡彩莉,刘杰瑞,雒聪文,王凯. 藏南羊卓雍错沉积物元素地球化学记录的过去2000年环境变化[J]. 地理学报, 2019, 74(7): 1345-1362.
[3]	潘汉雄,朱国锋,张昱,郭慧文,雍磊磊,万巧卓,马惠莹,李森. 中国耕地土壤相对湿度时空分异[J]. 地理学报, 2019, 74(1): 117-130.
[4]	范科科,张强,史培军,孙鹏,余慧倩. 基于卫星遥感和再分析数据的青藏高原土壤湿度数据评估[J]. 地理学报, 2018, 73(9): 1778-1791.
[5]	李勤,张强,黄庆忠,史培军. 中国气象农业非参数化综合干旱监测及其适用性[J]. 地理学报, 2018, 73(1): 67-80.
[6]	张蕾, 吕厚荃, 王良宇, 杨冰韵. 中国土壤湿度的时空变化特征[J]. 地理学报, 2016, 71(9): 1494-1508.
[7]	安文玲,刘晓宏,陈拓,徐国保,侯书贵,孙维贞. 云南丽江树轮δ¹⁸O记录的大气环流变化信息[J]. 地理学报, 2009, 64(9): 1103-1112.
[8]	李英年,王勤学,古松,伏玉玲,杜明远,赵亮,赵新全,于贵瑞. 高寒植被类型及其植物生产力的监测[J]. 地理学报, 2004, 59(1): 40-48.
[9]	谢安,孙永罡,白人海. 中国东北近50年干旱发展及对全球气候变暖的响应[J]. 地理学报, 2003, 58(7s): 75-82.
[10]	郭维栋,马柱国,姚永红. 近50年中国北方土壤湿度的区域演变特征[J]. 地理学报, 2003, 58(7s): 83-90.
[11]	翟盘茂,李晓燕. 中国北方沙尘天气的气候条件[J]. 地理学报, 2003, 58(7s): 125-131.
[12]	张伟强, 黄镇国. 中国热带的小冰期及其环境效应[J]. 地理学报, 2000, 55(6): 744-750.
[13]	周清波, 张丕远, 王铮. 合肥地区1736－1991年年冬季平均气温序列的重建[J]. 地理学报, 1994, 49(4): 332-337.
[14]	施少华, 杨怀仁, 王邨 . 中原地区晚全新世以来的环境变化 [J]. 地理学报, 1992, 47(2): 119-128.
[15]	张富国, 姚华栋, 张华林, 陈松 . 北京城区的降水与湿度分析 [J]. 地理学报, 1992, 47(2): 174-180.