全部 标题 作者
关键词 摘要

OALib Journal期刊
ISSN: 2333-9721
费用:99美元

查看量下载量

相关文章

更多...
冰川冻土  2013 

冰芯和气象记录揭示的青藏高原百年来典型冷暖时段气候变化特征

DOI: 10.7522/j.issn.1000-0240.2013.0153, PP. 1382-1390

Keywords: 青藏高原,冰芯记录,气象记录,冷期,暖期

Full-Text   Cite this paper   Add to My Lib

Abstract:

气候冷暖变化问题是全球科学家研究的一个聚焦点,但高海拔地区的气候变化过程尚不十分清楚,作为全球气候变化的敏感区的青藏高原更是如此.以青藏高原北部的古里雅冰芯、唐古拉冰芯和南部的达索普冰芯、宁金岗桑冰芯δ18O记录作为温度代用指标,同时结合青藏高原西北缘的吉尔吉斯斯坦Naryn站长期气象记录和北半球同时期的气温变化进行比较,研究了过去100a来青藏高原北部和南部的温度变化.结果显示青藏高原过去100a来共出现1910年左右、1920年左右、1950年左右、1970年代4个冷期,各冷期之间对应出现4次暖期,并且变冷的程度越来越弱而变暖的程度越来越强.其次,青藏高原气候的变冷变暖在不同地区和不同时段差异很大从空间尺度上看,青藏高原北部变暖过程比南部更强烈;从时间尺度上看,1910年左右和1920年左右的两次变冷十分明显,但1950年左右和1970年代的两次变冷不明显.另外,虽然有发生在1990年代早期的短暂降温过程,但与其说是一个冷事件,还不如说是一次变暖过程中的短暂停顿,随后表现为持续升温.

References

[1]  Ren Jiawen. Updating assessment results of global cryospheric change from SPM of IPCC WGI Fifth Assessment Report[J]. Journal of Glaciology and Geocryology,2013, 35(5): 1065-1067. [任贾文. 全球冰冻圈现状和未来变化的最新评估: IPCC WGI AR5 SPM 发布[J]. 冰川冻土, 2013, 35(5): 1065-1067.]
[2]  Shen Yongping, Wang Guoya. Key findings and assessment results of IPCC WGI Fifth Assessment Report[J].Journal of Glaciology and Geocryology,2013, 35(5): 1068-1076.[沈永平, 王国亚. IPCC第一工作组第五次评估报告对全球气候变化认知的最新科学要点[J]. 冰川冻土, 2013, 35(5): 1068-1076.]
[3]  Yao Tandong. Ice core study of the Tibetan Plateau[J]. Journal of Glaciology and Geocryology, 1998, 20(3): 233-237. [姚檀栋. 青藏高原冰芯研究[J]. 冰川冻土, 1998, 20(3): 233-237.]
[4]  Ye Duzheng.Tibetan Plateau Meteorology[M]. Beijing: Science Press,1979: 1-278.
[5]  Pan Baotian, Li Jijun. Qinghai-Tibetan Plateau: A driver and amplifier of the global climatic change—ⅡI. The effects of the uplift of Qinghai-Tibetan Plateau on climatic change[J]. Journal of Lanzhou University (Natural Sciences), 1996, 32(1): 108-115. [潘保田, 李吉均. 青藏高原: 全球气候变化的驱动机与放大器——Ⅲ. 青藏高原隆起对气候变化的影响[J]. 兰州大学学报(自然科学版), 1996, 32(1): 108-115.]
[6]  Wang Jie, He Xiaobo, Ye Baisheng, et al. Variations of albedo on the Dongkemadi Glacier, Tanggula Range[J]. Journal of Glaciology and Geocryology, 2012, 34(1): 21-28. [王杰, 何晓波, 叶柏生, 等. 唐古拉山冬克玛底冰川反照率变化特征研究[J]. 冰川冻土, 2012, 34(1): 21-28.]
[7]  Yao Tandong, Thompson L, Yang Wei, et al. Different glacier status with atmospheric circulations in Tibetan Plateau and surroundings[J]. Nature Climate Change, 2012, 2(9): 663-667.
[8]  Yao Tandong, Liu Xiaodong, Wang Ninglian, et al. Amplitude of climatic changes in Qinghai-Tibetan Plateau[J]. Chinese Science Bulletin, 2000, 45(13): 1236-1243.
[9]  Yao Tandong, Li Zhiguo, Yang Wei, et al. Glacial distribution and mass balance in the Yarlung Zangbo River and its influence on lakes[J]. Chinese Science Bulletin, 2010, 55(20): 2072-2078.
[10]  Duan Shuiqiang, Cao Guangchao, Liu Tao, et al. The recent expansion features and the cause of formation of the lakes in Qinghai Qiangtang Basin[J]. Journal of Glaciology and Geocryology,2013, 35(5): 1237-1247. [段水强, 曹广超, 刘 , 等. 青海羌塘盆地近期湖泊扩张特征及成因[J]. 冰川冻土, 2013, 35(5): 1237-1247.]
[11]  Wang Shaoling, Niu Fujun, Zhao Lin, et al. The thermal stability of roadbed in permafrost regions along Qinghai-Tibet Highway[J]. Cold Regions Science and Technology, 2003, 37(1): 25-34.
[12]  Wang Ninglian, Yao Tandong, Pu Jianchen, et al. Variations in air temperature during the last 100 years revealed by δ18O in the Malan ice core from the Tibetan Plateau[J]. Chinese Science Bulletin, 2003, 48(19): 2134-2138. [王宁练, 姚檀栋, 蒲健辰, 等. 青藏高原马兰冰芯记录的近百年来的气温变化[J]. 科学通报, 2003, 48(11): 1219-1223.]
[13]  Wang Youqing, Pu Jianchen, Zhang Yongliang, et al. Characteristic of present warming change recorded in Malan ice core, central Tibetan Plateau[J]. Journal of Glaciology and Geocryology, 2003, 25(2): 130-134. [王有清, 蒲健辰, 张永亮, 等. 马兰冰芯记录的青藏高原中部现代升温变化特征[J]. 冰川冻土, 2003, 25(2): 130-134.]
[14]  Tian Lide, Yao Tandong, Li Zhen, et al. Recent rapid warming trend revealed from the isotopic record in Muztagata ice core, eastern Pamirs[J]. Journal of Geophysical Research: Atmospheres, 2006, 111(D13), doi:10.1029/2005JD006249.
[15]  Zhang Yongjun, Kang Shichang, Qin Dahe, et al. Seasonal air temperature variations retrieved from a Geladandong Ice Core, Tibetan Plateau[J]. Acta Geographica Sinica,2007, 62(5): 501-509. [张拥军, 康世昌, 秦大河, 等. 青藏高原各拉丹冬冰芯记录的季节气温变化[J]. 地理学报, 2007, 62(5): 501-509.]
[16]  Yao Tandong, Guo Xuejun, Thompson L, et al.δ18Orecord and temperature change over the past 100 years in ice cores on the Tibetan Plateau[J]. Science in China (Series D: Earth Sciences), 2006, 49(1): 1-9. [姚檀栋, 郭学军, Thompson L, 等. 青藏高原冰芯过去100年δ18O记录与温度变化[J]. 中国科学(D辑: 地球科学), 2006, 36(1): 1-8.]
[17]  Wang Shaowu, Ye Jinlin, Gong Daoyi, et al. Construction of mean annual temperature series for the last one hundred years in China[J]. Quarterly Journal of Applied Meteorology,1998, 9(4): 392-401. [王绍武, 叶瑾琳, 龚道溢, 等. 近百年中国年气温序列的建立[J]. 应用气象学报, 1998, 9(4): 392-401.]
[18]  Dansgaard W. Oxygen-18 abundance in fresh water[J]. Nature, 1954, 174: 234-235.
[19]  Tian L, Yao T, Schuster P F, et al. Oxygen-18 concentrations in recent precipitation and ice cores on the Tibetan Plateau[J]. Journal of Geophysical Research: Atmospheres, 2003, 108(D9), doi:10.1029/2002JD002173.
[20]  Yao Tandong,Thompson L G, Mosley-Thompson E, et al. Climatological significance ofδ18O in north Tibetan ice cores[J]. Journal of Geophysical Research: Atmospheres, 1996, 101(D23): 29531-29537.
[21]  Tian Lide, Yao Tandong, Numaguti A, et al. Stable isotope variations in monsoon precipitation on the Tibetan Plateau[J]. Journal of the Meteorological Society of Japan (Ser. Ⅱ), 2001, 79(5): 959-966.
[22]  Tian Lide, Yao Tandong, Numaguti A, et al. Relation between stable isotope in monsoon precipitation in southern Tibetan Plateau and moisture transport history[J]. Science in China (Series D: Earth Sciences), 2001, 44(S1): 267-274. [田立德, 姚檀栋, 孙维贞, 等. 青藏高原南北降水中δD和δ18O关系及水汽循环[J]. 中国科学(D辑: 地球科学), 2001, 31(3): 214-220.]
[23]  Thompson L G, Yao T, Mosley-Thompson E, et al. A high-resolution millennial record of the South Asian monsoon from Himalayan ice cores[J]. Science, 2000, 289(5486): 1916-1919.
[24]  Tian Lide, Yao Tandong, Yang Zhihong, et al. A 4-year's study on oxygen isotope in precipitation at Tuotuohe Meteorological Station, Tibetan Plateau[J]. Journal of Glaciology and Geocryology, 1998, 20(4): 438-443.
[25]  Joswiak D R, Yao T, Wu G, et al. A 70-yr record of oxygen-18 variability in an ice core from the Tanggula Mountains, central Tibetan Plateau[J]. Climate of the Past, 2010, 6(2): 219-227.
[26]  Zhao Huabiao, Xu Baiqing, Yao Tandong, et al. Deuterium excess record in a southern Tibetan ice core and its potential climatic implications[J]. Climate Dynamics, 2012, 38(9/10): 1791-1803.
[27]  Lin Zhenyao, Zhao Xinyi. Spacial characteristics of changes in temperature and precipitation of the Qinghai-Xizang (Tibet) Plateau[J]. Science in China (Series D: Earth Sciences), 1996, 39(4): 442-448. [林振耀, 赵昕奕. 青藏高原气温降水变化的空间特征[J]. 中国科学(D辑: 地球科学), 1996, 26(4): 354-358.]
[28]  Cheng Guodong, Li Shuxun, Liu Xiaodong. Recent climatic warming over the Qinghai-Xizang (Tibet) Plateau and its influences on environments[J]. Chinese Science Bulletin, 1999, 44(S1): 264.
[29]  Liu Xiaodong, Chen Baode. Climatic warming in the Tibetan Plateau during recent decades[J]. International Journal of Climatology, 2000, 20(14): 1729-1742.

Full-Text

Contact Us

service@oalib.com

QQ:3279437679

WhatsApp +8615387084133