地球科学进展 ›› 2006, Vol. 21 ›› Issue (12): 1314 -1323. doi: 10.11867/j.issn.1001-8166.2006.12.1314

所属专题: 青藏高原研究——青藏科考虚拟专刊

研究论文 上一篇    下一篇

青藏高原降水中稳定氧同位素研究进展
余武生 1,2,田立德 1,2,马耀明 1,2,尹常亮 2   
  1. 1. 中国科学院青藏高原研究所青藏高原环境与过程实验室,北京 100085;2. 中国科学院寒区旱区环境与工程研究所冰冻圈与环境联合重点实验室,甘肃 兰州 730000
  • 收稿日期:2006-10-11 修回日期:2006-10-31 出版日期:2006-12-15
  • 通讯作者: 余武生 E-mail:yuws@itpcas.ac.cn
  • 基金资助:

    国家自然科学基金项目“东亚季风系统与降水中稳定同位素研究”(编号:40571039);国家自然科学基金创新群体项目“冰芯与寒区环境”(编号:40121101);国家重点基础研究发展计划项目“青藏 高原环 境变 化的机制”(编号:2005CB422004);GAME /Tibet和 CAMP /Tibet计划资助.

Advances in the Study of Stable Oxygen Isotope in Precipitation on the Tibetan Plateau

Yu Wusheng 1,2,Tian Lide 1,2,Ma Yaoming 1,2,Yin Changliang 2
  

  1. 1.Laboratory of Environment and Process on Tibetan Plateau,Institute of Tibetan Plateau Research,Chinese Academy of Sciences,Beijing 100085,China;2.Key Laboratory of Cryosphere and Environment,Cold and Arid Regions Environmental and Engineering Research Institute,Chinese Academy of Sciences,Lanzhou 730000,China
  • Received:2006-10-11 Revised:2006-10-31 Online:2006-12-15 Published:2006-12-15

稳定氧同位素(δ18O)在冰芯研究中能够很好地反映气候变化,尤其是气温变化的一项重要指标。研究青藏高原降水中δ18O为科学的解释冰芯中δ18O记录具有重要的指示意义。分别介绍了青藏高原季风区、非季风区以及季风区和非季风区的过渡区降水中δ18O研究历史和现状,并对该领域未来的研究趋势进行了展望。

Stable oxygen isotope(δ18O)in ice core records is good proxy for temperature record and is representative of climatic change. The study of the δ18O variation in precipitation can throw light on the climatic significance of δ18O records in ice core. This paper reviews the advances in the study of stable oxygen isotope in precipitation in the monsoon region,the non-monsoon region,and the transition region between the monsoon region and the non-monsoon region on the Tibetan Plateau,respectively. Moreover,an outlook on future research over the Tibetan Plateau is presented in this paper.

中图分类号: 

[1] Dansgaard W. The abundance of 18O in atmospheric water and water vapor[J].Tell us,1953,5(4):461-469 .

[2] Epstein S, Mayeda T. Variation of 18O content of waters from natural sources [J]. Geochimica et Cosmochimica Acta,1953,4 :213-224 .

[3] Friedman I. Deuterium content of natural water and other substances[J]. Geochimica et Cosmochimica Acta,1953,4 :89-103 .

[4] Dansgaard W. Stable isotopes in precipitation[J]. Tellus,1964,16(4):436-468.

[5] Epstein S, Sharp R P. Six-year record of oxygen and hydrogen isotope variations in South Pole firn[J]. Journal of Geogphysical Research,1965,70(8):1 809-1 814.

[6] Gonfiantini R. Some Results on oxygen isotope stratigraphy in the deep drilling at King Baudou in Station, Antarctica[J]. Journal of Geogphysical Research,1965,70(8):1 815-1 819.

[7] Yu Jinsheng,Yu Fuji,Liu Deping. The oxygen and hydrogen isotopic compositions of meteoric waters in the eastern part of China[J]. Geochimica,1987,1:22-26.[于津生,虞福基,刘德平.中国东部大气降水氢、氧同位素组成[J]. 地球化学,1987,1:22-26.]

[8] Yu Jinsheng, Zhang Hongbin, Yu Fuji, et al. Oxygen isotopic composition of meteoric water in the eastern part of Xizang [J].Geochimica,1980,2:113-121.[于津生,张鸿斌,虞福基,. 西藏东部大气降水氧同位素组成特征[J]. 地球 化学,1980,2:113 -121.]

[9] Wei Keqin,Lin Ruifen,Wang Zhixiang. Hydrogen and oxygen stable isotopic composition and tritium content of waters from Yangbajin geothermal area, Xizang, China [J]. Geochimica,1983,4:338-346 .[卫克勤,林瑞芬,王志祥. 西藏羊八井地热水的氢、氧稳定同位素组成及氚含量[J]. 地球化学,1983,4:338-346 .]

[10] Zheng Shuhui,Hou Fagao,Ni Baoling. Research on the hydrogen and oxygen stable isotope of precipitation in China[J]. Chinese Science Bulletin,1983,28(13):801-806 .[郑淑蕙,侯发高,倪葆龄. 我国大气降水的氢氧稳定同位素研究[J]. 科学通报,1983,28(13):801-806.]

[11] Yao Tandong,Xie Zichu,Wu Xiaoling,et al. Climatic change since Little Ice Age recorded by Dunde ice cap [J]. Science in China(Series B),1991,34(6):760-767.

[12] Yao Tandong,Jiao Keqin,LiZhongqin,et al. Climatic and environmental records in Guliya Ice Cap [J]. Science in China(Series B),1994,24(7):766-773.[姚檀栋,焦克勤,李忠勤,. 古里雅冰帽气候环境记录[J]. 中国科学:B ,1994,24(7):766 -773.]

[13] Yao Tandong, Thompson L G, Mosley-Thompson E, et al. Climatological significance of δ18O in north Tibetan ice cores[J].Journal of Geophysical Research,1996,101( D23): 29 531-29 537.

[14] Hou Shugui,Qin Dahe,Wake C P,et al. Climatological significance of ice core net-accumulation record at Mt. Qomolangma(Everest)[J].Chinese Science Bulletin,2000,45(3):259-264.

[15] Thompson L G, Yao Tandong, Mosley-Thompson E, et al. A High-Resolution Millennial Record of the South Asian Monsoon from Himalayan Ice Cores[J]. Science,2000,289:1 916-1 919.

[16] 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):2 134-2 138.

[17] Hou Shugui,Zhang Dongqi. Comparison of two ice core records since 1954 from Mt. Qomolangma(Everest) region[J]. Journal of Glaciology and Geocryology,2003,25(3):256-260. [侯书贵,张东启. 1954年以来珠穆朗玛峰地区两支冰芯记录的对比分析[J]. 冰川冻土,2003,25(3):256-260.]

[18] Tian Lide,Yao Tandong,LiZhen,et al. Recent rapid warming trend revealed from the isotopic record in Muztagata ice core,eastern Pamirs[J]. Journal of Geophysical Research,2006,111:D13103,doi:10.1029 /2005JD006249.

[19] Yao Tandong,Guo Xuejun,Thompson L,et al.δ18O record and temperature change over the past 100 years in ice cores on the Tibetan Plateau [J]. Science in China(Series D),2006,49(1):1 -9.

[20] Zhang Xinping,Shi Yafeng,Yao Tandong. Variational features of precipitation δ18O in Northeast Qinghai-Tibet Plateau [J]. Science in China(Series B),1995,38(7):854-864.

[21] Yu Wusheng,Yao Tandong,Tian Lide,et al. Variation ofδ18O in precipitation in the western Tibetan plateau[J]. Journal of Glaciology and Geocryology,2004,26(2):146-152.[余武生,姚檀栋,田立德,. 青藏高原西部降水中δ18O 变化特征[J]. 冰川冻土,2004,26(2):146-152.]

[22] Tian Lide,Yao Tandong,Shen Yongping,et al. Study on stable isotope in river water and precipitation in Naqu River basin, Tibetan Plateau [J]. Advances in Water Science,2002,13(2):206-210.[田立德,姚檀栋,沈永平,. 青藏高原那曲河流域降水及河流水体中氧稳定同位素研究[J]. 水科学进展,2002,13(2):206 -210 .]

[23] Tian Lide,Yao Tandong,Yang Zhihong,et al. Characteristics of Proceedings of δ18O in precipitation and glacial meltwater at Tanggula Mountains observed in the late summer of 1993[C]Proceedings of the Fifth Chinese Conference on Glaciology and Geocryology(Vol.1). Lanzhou:Gansu Culture Press,1996:190-196 .[田立德,姚檀栋,杨志红,. 唐古拉山1993年夏末降水及冰川融水中δ18O 变化特征[C]∥第五届全国冰川冻土学大会论文集( ). 兰州:甘肃文化出版社,1996 :190-196 .]

[24] Tian Lide,Yao Tandong,Zhang Yinsheng,et al. Chemical characteristics of summer precipitation at Xixiabangma, Tibetan Plateau[J]. Chinese Journal of Environment Science,1998,19(6):1-5.[田立德,姚檀栋,张寅生,. 希夏邦马夏季降水中水化学特征[J]. 环境科学,1998,19(6):1-5.]

[25] Kang Shichang,Qin Dahe,Yao Tandong,et al. Characteristics of δ18O in precipitation during summer monsoon season in high elevation of the Dasuopu glacier, Mount Xixiabangma[J]. Journal of Mountain Science, 2000, 18(1):1-6. [康世昌,秦大河,姚檀栋,. 希夏邦马峰达索普冰川高海拔区夏季风期间大气降水的δ18O 特征[J]. 山地学报, 2000, 18(1):1 -6.]

[26] Kang Shichang,Kreutz Karl J,Mayewski Paul A,et al. Stable-isotopic composition over the northern slope of the central Himalayas[J]. Journal of Glaciology,2002,48(163):519 -526 .

[27] Hou Shugui, Valerie Masson-Delmotte, Qin Dahe, et al. Modern precipitation stable isotope vs. elevation gradients in the High Himalaya. Comment on “A new approach to stable isotope-based paleoaltimetry: Implications for paleoaltimetry and paleohypsometry of the High Himalaya since the Late Miocene” by David B.Rowley,et al.[Earth Planetary Science Letters,2001,188:253-268]. Earth Planetary Science Letters,2003,209(3 /4):395-399 .

[28] Li Zhen,Yao Tandong,Tian Lide,et al. Variations of δ18O in precipitation from the Muztagata Glacier, East Pamirs[J]. Science in China(Series D),2006,49(1):36-42.

[29] Yu W usheng,Yao Tandong,Tian Lide,et al. Relationships of δ18O in summer precipitation and temperature and moisture trajectories in Muztagata, western China[J]. Science in China(Series D),2006,49(1):27-35.

[30] Wang Jun,Liu Tianchou,Yin Guan. Characteristics of isotope distribution in precipitation in the middle-lower reaches of Yarlung Zangbo River[J]. Geology-Geochemistry,2000,28(1):63-67.[王军,刘天仇,尹观. 西藏雅鲁藏布江中、下游地区大气降水同位素分布特征[J]. 地质地球化学,2000,28(1):63-67.]

[31] Ning Aifeng,Yin Guan,Liu Tianchou. Characteristics of isotope distribution of atmospheric precipitation in the Lasa River area[J]. Journal of Mineralogy and Petrology,2000,20(3):95-99 .[宁爱风,尹观,刘天仇. 拉萨河地区的大气降水同位素分布特征[J]. 矿物岩石,2000,20(3):95-99.]

[32] Hubner H,Kowski P,Hermichen W D,et al. Regional and temporal variations of Deuterium in the precipitation and atmospheric moisture of central Europe[C]Isotope Hydrology 1978.Vienna/Austria:IAEA-publications, 1979:289-307.

[33] Schoch-Fischer H,Rozanski K,Jacob H,et al. Hydrom eteorological factors controlling the time variation of D,18O and 3H in atmospheric water vapour and precipitation in the northern westwind belt[C]Isotope Hydrology 1983. Vienna/Austria:IAEA -publications,1984:3-30.

[34] Yu Wusheng,Yao Tandong,Tian Lide,et al. Isotopic com position of atmospheric water vapor before and after the monsoon’s end in the Nagqu River Basin[J]. Chinese Science Bulletin,2005,50 (23):2 755 -2 760.

[35] Yao Tandong,Thompson L G,Jiao Keqin,et al. Recent warming as recorded in the Qinghai Tibetan cryosphere[J]. Annals of Glaciology,1995,21:19 6-200.

[36] He Yuanqin,Pang Hongxi,Lu Aigang,et al. Spatial and temporal variations of the stable isotopes in snow packs and glacial runoff in different types of glacier areas in China [J]. Journal of Glaciology and Geocryology, 2006, 28(1):22-28. [何元庆,庞洪喜,卢爱刚,. 中国西部不同类型冰川区积雪及其融水径流中稳定同位素比率的时空变化及其气候效应[J]. 冰川冻土,2006,28(1):22-28.]

[37] Thompson L G,Mosely-Thompson E,Davis M E,et al. Holocene-Late Pleistocene climate ice core records from Qinghai-Tibetan Plateau [J]. Science,1989,246:474 -477.

[38] Thompson L G,Mosley-Thompson E,Davis M E,et al. Recent warming:Ice core evidence from tropical ice cores with emphasis up on Cenral Asia[J]. Global and Planetary Change,1993,7 :145 -156.

[39] Yao Tandong,Thompson L G. Trends and features of climatic changes in the past 5 000 years recorded by the Dunde ice core[J]. Annals of Glaciology,1992,16:21-24.

[40] Yao Tandong,ShiYafeng,Thompson L G. High resolution record of paleoclimate since the little ice age from the Tibetan ice cores[J]. Quaternary International,1997,37 :19-23.

[41] Wang Ninglian,Yao Tandong,Pu Jianchen,et al. Climatic and environmental changes during the last 1 000 years revealed byδ18O in the Malan ice core from the northern Tibetan Plateau[J]. Science in China(Series D), 2006, 36(8):723-732.[王宁练,姚檀栋,蒲建辰,. 青藏高原北部马兰冰芯记录的近千年来气候环境变化[J]. 中国科学:D ,2006,36(8):723-732 .]

[42] Wang Ninglian,Thompson L G ,Davis M E ,et al. Influence of variations in NAO and SO on air temperature over the northern Tibetan Plateau as recorded by δ18O in the Malan ice core[J].Geophysical Research Letters, 2003, 30(22),2167,doi:10.10 29 /2003 GL018188 .

[43] Wang Ninglian. Decrease trend of dust event frequency over the past 200 years recorded in the Malan ice core from the northern Tibetan Plateau[J]. Chinese Science Bulletin,2005,50(24):2 866-2 871.

[44] Xiang Shurong,Yao Tandong,An Lizhe,et al. Change of bacterial community in the Malan ice core and its relation to climate and environment[J]. Chinese Science Bulletin,2004,49(17):1 869-1 875.

[45] Yao Tandong,Ding Liangfu,Pu Jianchen,et al. Characteristic of δ18O in snow and its relation with moisture sources in Tanggula Mountains,Tibetan Plateau[J]. Chinese Science Bulletin,1991,36 (20):1 570-1 573 .[姚檀栋,丁良福,蒲建辰,. 青藏高原唐古拉山地区降雪中δ18O 特征及其与水汽来源的关系[J]. 科学通报,1991,36(20):1 570-1 573.]

[46] Tian Lide,Yao Tandong,Schuster P F,et al. Oxygen-18 concentrations in recent precipitation and ice cores on the Tibetan Plateau[J]. Journal of Geophysical Research,2003,108(D9):ACH16-1- ACH16-10.

[47] Tian Lide,Yao Tandong,White J C W,et al. Westerly moisture transport to the middle of Himalayas revealed from the high deuterium excess[J]. Chinese Science Bulletin,2005,50(10):1 026-1 030 .

[48] Tian Lide,Yao Tandong,Yu Wusheng,et al. Stable isotopes of precipitation and ice core on the Tibetan Plateau and moisture transports[J]. Quaternary Sciences,2006,26(2):145-152.[田立德,姚檀栋,余武生,. 青藏高原水汽输送与冰芯中稳定同位素记录[J]. 第四纪研究,2006,26(2):145-152.]

[49] Duan Keqin,Yao Tandong. Monsoon variability in the Himalayas under the condition of global warming[J]. Journal of Meteorology Society Japan,2003,81(2):251 -257.

[50] Zhang Dongqi,Qin Dahe,Hou Shugui,et al. Climatic significance of the δ18O records from an 80.36 m ice core in the East Rongbuk Glacier,Mount Qomolangma(Everest) [J]. Science in China(Series D),2005,48(2):266-272.

[51] Hou Shugui,Qin Dahe,Zhang Dongqi,et al. Comparison of two ice core chemical records recovered from the Mt. Qomolangma(Everest) region [J]. Annals of Glaciology,2002,35:266-272.

[52] Tian Lide,Yao Tandong,Yang Zhihong. Spatial distribution of δ18O in precipitation over the Qinghai-Xizang Plateau and its controlling factors[C]Annual Report on the Study of the Formation, Evolution, Environmental Variations and Ecosystem on the Qinghai-Tibetan Plateau(1995). Beijing:Science Press,1995:243-250.[田立德,姚檀栋,杨志红. 青藏高原降水中δ18O的空间分布特征及其影响因素[C]∥青藏高原形成演化、环境变迁和生态系统研究学术年刊(1995).北京:科学出版社,1995:243-250.]

[53] Liu Xiaodong,Hou Ping. Variation of summer rainfall over Qinghai-Xizang Plateau and its association with the North Atlantic Oscillation[J]. Acta Meteorologica Sinica,1999,57(5):561-57.[刘晓东,侯萍. 青藏高原中东部夏季降水变化及其与北大西洋涛动的联系[J]. 气象学报,1999,57(5):561-570.]

[54] Wang Ninglian. The boundary between the northern and southern Tibetan Plateau with different variations in the warm season air temperatures on the decadal time scale[J]. Quaternary Sciences,2006,26(2):165-172. [王宁练. 青藏高原南部和北部暖季气温年代际变化差异的界线位置[J]. 第四纪研究,2006,26(2):165-172.]

[55] Yu Wusheng,Yao Tandong,Tian Lide,et al. Oxygen-18 isotopes in precipitation on the eastern Tibetan Plateau[J]. Annals of Glaciology,2006,43:263-268.

[56] 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),2001,44(suppl.):267-274.

[57] Aragus-Aragus L,Froehlich K,Rozanski K. Stable isotope composition of precipitation over southeast Asia [J]. Journal of Geophysical Research,1998,103(D22):28 721-28 742.

[58] Johnson K R,Ingram B L. Spatial and temporal variability in the stable isotope systematics of modern precipitation in China: Implications for paleoclimatic reconstructions[J]. Earth Planetary Science Letters, 2004, 220:365-377 .

[59] Yao Tandong,Liu Xiaodong,Wang Ninglian. The question of the range of climatic change on the Qinghai-Tibetan Plateau[J]. Chinese Science Bulletin,2000,45(1):98-105.[姚檀栋,刘晓东,王宁练. 青藏高原地区的气候变化幅度问题[J]. 科学通报,2000,45(1):98-105.]

[60] Yao Tandong. Abrupt climatic changes on the Tibetan Plateau during the Last Ice Age-comparative study of the Guliyaice core with the Green land GRIP ice core[ J]. Science in China(Series D),1999,42(4):358-368 .

[61] Zhang Xinping,Yao Tandong,Jin Huijun. The influence of ENSO event on the modern δ18O in the Guliya ice core[J]. Journal of Glaciology and Geocryology,2000,22(1):23-28 . [章新平,姚檀栋,金会军. ENSO 事件对青藏高原古里雅冰芯中现代δ18O 的影响[J]. 冰川冻土,2000,22(1):23-28. ]

[62] Yang Meixue,Yao Tandong,He Yuanqing,et al. ENSO events recorded in the Guliya ice core[J]. Climatic Change, 2000,47:401-409 .

[63] Yang Meixue,Yao Tandong. The response of the climate records in the Guliya ice core to ENSO events[J]. Journal of Glaciology and Geocryology,2003,25(1):27-33. [杨梅学,姚檀栋. 古里雅冰芯气候记录对ENSO事件的响应[J]. 冰川冻土,2003 ,25(1):27-33 .]

[64] Zhang Xinping,Liu Jingmiao,He Yuanqing,et al. Humidity effect and its influence on the seasonal distribution of precipitation δ18O in monsoon regions[J]. Advances in Atmospheric Sciences,2005,22(2):271-277 .

[65] Tian Lide,Yao Tandong,Pu Jianchen,et al. Characteristics of δ18O in Summer Precipitation at Lhasa[J].Journal of Glaciology and Geocryology,1997,19(4):295-301.[田立德,姚檀栋,蒲建辰,. 拉萨夏季降水中氧稳定同位素变化 特征[J].冰川冻土,1997,19(4):295-301.]

[66] Tian Lide,Yao Tandong,Sun Weizhen,et al. Stable isotope variation of precipitation in the middle of Qinghai-Xizang Plateau and monsoon activity [J]. Geochimica,2001,30(3):217-222. [田立德,姚檀栋,孙维贞,. 青藏高原中部降水稳定同位素变化与季风活动[J].地球化学,2001,30(3):217-222 .]

[67] Tian Lide,Yao Tandong,Numaguti A,et al. Stable Isotope Variations in Monsoon Precipitation on the Tibetan Plateau [J].Journal of Meteorology Society of Japan,2001,17(5):959-966 .

[68] Zhang Xinping,Shi Yafeng,Yao Tandong. Relation between δ18O in atmospheric precipitation and temperature and precipitation[J].Chinese Geographical Science,1995,5(4):289-299.

[69] Yao Tandong,Masson V,Jouzel J,et al. Relationships between δ18O in precipitation and surface air temperature in the Urumqi River Basin, east Tianshan Mountains, China[J].Geophysical Research Letters,1999,26(23):3 473-3 476.

[70] Zhang Xinping,Nakawo M,Yao Tandong,et al. Variations of stable isotopic compositions in precipitation on the Tibetan Plateau and its Adjacent Regions[J]. Science in China(Series D),2002,45(6):481-493.

[71] Tian Lide,Masson-Delmotte V,Stievenard M,et al. Tibetan plateau summer monsoon northward extent revealed by measurements of water stable isotopes [J]. Journal of Geophysical Research,2001,106(D22):28 081-28 088 .

[72] Yao Tandong, Qin Dahe, Xu Baiqing, et al. Temperature change over the past millennium recorded in ice cores from the Tibetan Plateau[J]. Advances in Climate Change Research,2006,2(3):99-103 .[姚檀栋,秦大河,徐柏青,. 冰芯记录的过去1 000 年青藏高原温度变化[J]. 气候变化研究进展,2006,2(3):99-103.]

[73] Jouzel J, Lorius C, Petit J R, et al. Vostok ice core:A continuous isotope temperature record over the last climatic cycle(160 000 years)[J]. Nature,1987,329:403-408.

[1] 兰爱玉, 林战举, 范星文, 姚苗苗. 青藏高原北麓河多年冻土区阴阳坡地表能量和浅层土壤温湿度差异研究[J]. 地球科学进展, 2021, 36(9): 962-979.
[2] 王澄海, 张晟宁, 张飞民, 李课臣, 杨凯. 论全球变暖背景下中国西北地区降水增加问题[J]. 地球科学进展, 2021, 36(9): 980-989.
[3] 仲雷,葛楠,马耀明,傅云飞,马伟强,韩存博,王显,程美琳. 利用静止卫星估算青藏高原全域地表潜热通量[J]. 地球科学进展, 2021, 36(8): 773-784.
[4] 王慧,张璐,石兴东,李栋梁. 2000年后青藏高原区域气候的一些新变化[J]. 地球科学进展, 2021, 36(8): 785-796.
[5] 田凤云,吴成来,张贺,林朝晖. 基于 CAS-ESM2的青藏高原蒸散发的模拟与预估[J]. 地球科学进展, 2021, 36(8): 797-809.
[6] 马宁. 40年来青藏高原典型高寒草原和湿地蒸散发变化的对比分析[J]. 地球科学进展, 2021, 36(8): 836-848.
[7] 柯思茵,张冬丽,王伟涛,王孟豪,段磊,杨敬钧,孙鑫,郑文俊. 青藏高原东北缘晚更新世以来环境变化研究进展[J]. 地球科学进展, 2021, 36(7): 727-739.
[8] 魏梦美,符素华,刘宝元. 青藏高原水力侵蚀定量研究进展[J]. 地球科学进展, 2021, 36(7): 740-752.
[9] 王忠静,石羽佳,张腾. TRMM遥感降水低估还是高估中国大陆地区的降水?[J]. 地球科学进展, 2021, 36(6): 604-615.
[10] 李耀辉, 孟宪红, 张宏升, 李忆平, 王闪闪, 沙莎, 莫绍青. 青藏高原—沙漠的陆—气耦合及对干旱影响的进展及其关键科学问题[J]. 地球科学进展, 2021, 36(3): 265-275.
[11] 杨军怀,夏敦胜,高福元,王树源,陈梓炫,贾佳,杨胜利,凌智永. 雅鲁藏布江流域风成沉积研究进展[J]. 地球科学进展, 2020, 35(8): 863-877.
[12] 王鹏,刘磊,刘西川,胡帅,赵世军,姬文明,高太长. 球载云降水粒子探测器研究现状及进展[J]. 地球科学进展, 2020, 35(7): 704-714.
[13] 姚天次,卢宏玮,于庆,冯玮. 50年来青藏高原及其周边地区潜在蒸散发变化特征及其突变检验[J]. 地球科学进展, 2020, 35(5): 534-546.
[14] 张宏文,续昱,高艳红. 19822005年青藏高原降水再循环率的模拟研究[J]. 地球科学进展, 2020, 35(3): 297-307.
[15] 苗毅, 刘海猛, 宋金平, 戴特奇. 青藏高原交通设施建设及影响评价研究进展[J]. 地球科学进展, 2020, 35(3): 308-318.
阅读次数
全文


摘要