All Title Author
Keywords Abstract

冰川冻土  1998 

青藏高原冰芯研究

, PP. 233-237

Keywords: 青藏高原,冰芯研究,成果总结,未来战略

Full-Text   Cite this paper   Add to My Lib

Abstract:

冰芯研究是全球变化研究的重要内容之一.冰芯因其分辨率高、信息量大、保真性强、时间序列长和洁净度高而成为研究地球系统中生物、化学和物理过程的最好媒体.文章首先阐述了青藏高原冰芯研究的基本内容,即与冰芯研究相关的过程研究和冰芯记录研究.然后对近10多年来青藏高原冰芯研究的主要成果进行了总结,并将青藏高原冰芯研究的主要成果归纳为5个方面.同时指出青藏高原冰芯研究在8个方面取得了突破性的进展.最后,从野外工作和实验室工作两个方面对未来青藏高原冰芯研究的实施战略进行了阐述.

References

[1]  Yao Tandong, Thompson Lonnie G, Ellen Mosley- Thompson et al, 1996a Climatological significance of δ18O in north Tibetan ice core Journal of Geophysical Research, 101(D23):29 531~29 537
[2]  Savoie D L,Prospero J M,Nees R T,1987.Nitrate,Non-sea-salt sulfate,and mineral aerosol over th e Northw estern Indian Ocean.Journal of Geoph ysical Research,92(D1):933~942
[3]  Cerling T E, 1993.Expansion of C4 ecosystems as an indicater of global ecological change in the late Miocene.Nature, 361:344~345
[4]  Yao Tandong, Thompson Lonnie G, Yang Zhihong et al,1996b Processes coupling climatic and environmental variations revealed from Guliya ice core Cryosplere, 2:25~32
[5]  Chen Haowen et al.,1990. Microbes in the surface water of the shoaling areas of the Antarctic krill and their ecological analysis. Collected Oceanic Works,13(2):85~99
[6]  Spicer C W,1982.Nitrogen oxide reactions in the urban plume of Boston.Science,215(4 536):1 095~1 098
[7]  Yao Tandong, Pu Jianchen, Sheng Wenkun et al, 1996c Chemistry of snow and ice on the Tibetan Plateau, 2:20~24
[8]  Chappellaz J, 1994.Synchronous change in at mospheric CH4 and Greenland climate between 40 and 8kyr B.P.Nature, 366:443~445
[9]  Chen Haowen et al.,1993. State Antarctic Committee. Investigation report of 9f CHINARE and global gravity.China Ocean Press,Beijing, 93~103 (in Chinese)
[10]  Suess H E,1965.Secular variations of the cosmic-ray-produced Carbon-14 in the atmosphere and their interpretation.Journal of Geo-physical Research,70(23):5 937~5 952
[11]  Yao Tandong, Thompson Lonnie G, Qin Dahe et al, 1996d Variations in temperature and precipitation in the past 2000 years on the Xizang(Tibet) Plateau Guliya ice core record Science in China, 39:425~433
[12]  Chen Haowen et al.,1994. Microbes in the area of the South Shetland Islands. Antarctic Res.,5(2):9~17
[13]  Yao Tandong, Yang Zhihong, Kang Xingcheng et al,1996e Variations of Cryosphere and Atmosphere on the Tibetan Plateal Cryosphere, 2:1~6
[14]  Cole D R, Monger H C, 1994.Influence of atmospheric CO2 on the decline of C4 plants during the last deglaciation.Nature, 368:533~ 536
[15]  Talbot R W,Harriss R C,Brow ell E V et al.,1986.Distribution and geoch emistry of Aerosols in the tropical North Atlantic troposphere:relationship to Saharan dust.Journal of Geophysical Research,91(D4):5 173~5 182
[16]  Yao Tandong, Yang Zhihong, Kang Xingcheng et al, 1996f Variations of Cryosphere and Atmosphere on the Tibetan Plateau Cryosphere, 2:1~6
[17]  State Technological Superintendency Administration, 1991.National Standards of Peoples Republic of China. Offshore pollution survey and biological monitoring, In specifications of oceanographic survey. China Ocean Press,Beijing, 627~730 (in Chinese)
[18]  Thompson L G,Thompson E M,Davis M E et al.,1990.Glacial stage ice-core records from the subtropical Dunde Ice Cap,China.Annals of Glaciology,14:288~297
[19]  Yao Tandong, Shi Yafeng, Thompson Lonnie G, 1997 High resolation record of Paleoclimate since the Little Ice Age from the Tibetan ice cores Quaternary International, 37:19~23
[20]  Dansgaard W, Johnse S J, Clausen H B et al., 1993.Evidence for general instability of past climate from a 250 kyrice core record. Nature, 364:218~220
[21]  Thompson L G,Thompson E M,Davis M E et al.,1995.Late glacial stage and Holocene tropical ice core records from Huascaran,Peru.Science,269:46~50
[22]  Wheeler P A, Kirohaman D L,1986. Utilization of inorganic and organic forms of nitrogen by bacteria in marine systems. limnol Oceanol,31(5):998~1 009
[23]  Zh ang Xinping, Shi Yafeng, Yao Tandong, 1995 Variational feature of Precipitation δ18O in Northeast Qinghai-Tibet Dlateau Science in China(Series B), 854~864

Full-Text

comments powered by Disqus

Contact Us

service@oalib.com

QQ:3279437679

微信:OALib Journal