強明瑞

強明瑞

男,1973年7月出生,山西中陽人,博士,自然地理研究所教授。研究方向為乾旱區環境演變

湖泊沉積與大氣粉塵。近年來,主要探討了末次冰期以來騰格里沙漠東南緣風成沉積與沙漠環境演化,末次冰消

期東亞季風西北緣區氣候快速變化事件;利用蘇干湖沉積重建近8 ka來氣候變化序列,著重探討了2 ka來氣候變化歷史;初步理解了柴達木盆地封閉湖泊沉積記錄塵暴事件與源區粉塵釋放的模式、重建了柴達木盆地全新 世塵暴演化歷史。主持國家自然科學基金項目、中國博士后科學基金各1項,經費30餘萬元,參加國家自然科學基金、“973”等項目5項,發表論文10餘篇,獲中國地理學會青年優秀論文獎1項。

學習工作經歷


1992.9~1996.7 山西師範大學地理系 本科
1999.9~2002.12 蘭州大學 自然地理學 博士
2003.7~2005.9 北京師範大學 地理學 博士后研究
2005.9~2008 蘭州大學資源環境學院/西部環境教育部重點實驗室 副教授
2008至今 蘭州大學資源環境學院/西部環境教育部重點實驗室 教授

在研項目


1.“新世紀優秀人才支持計劃”,教育部,50萬元,負責人;
2.“創新群體”項目第一期、第二期與第三期:青藏高原和中東亞乾旱區環境變化與地表過程研究(批准號:40421101,40721061),2005.1-2011.12,國家自然科學基金委,20萬元,主要參加者;
3.世界各地黃土磁化率與古氣候不同關係機制以及古氣候重建問題系統研究(No. 40830105),2009.1-2012.12,國家自然科學基金重點項目,165萬元,主要參加者;
4.國家“973”項目,黃河上游沙漠寬谷段風沙水沙過程與調控機理(No. 2011CB403300)。第一課題“黃河上游沙漠寬谷段粗沙來源與沉積時空特徵(No. 2011CB403301)”,2011.1-2015.12,475萬元,主要參加人;

發表論文


1.Mingrui Qiang, Fahu Chen, Zhenting Wang, Guangming Niu, Lei Song, 2010. Aeolian deposits at the southeastern margin of the Tengger Desert (China): Implications for surface wind strength in the Asian dust source area over the past 20,000 years. Palaeogeography, Palaeoclimatology, Palaeoecology 286, 66-80.
2. Qiang, M.,Lang, L., Wang, Z., 2010. Do fine-grained components of loess indicate westerlies: Insights from observations of dust storm deposits at Lenghu (Qaidam Basin, China). Journal of Arid Environments 74, 1232-1239.
3. Mingrui Qiang, Fahu Chen, Jiawu Zhang, Ruiping Zu, Ming Jin, Aifeng Zhou, Shun Xiao, 2007. Grain size in sediments from Lake Sugan: a possible linkage to dust storm events at the northern margin of the Qinghai–Tibetan Plateau. Environmental Geology 51(7), 1229-1238.
4. Mingrui Qiang, Fahu Chen, Aifeng Zhou, Shun Xiao, Jiawu Zhang, Zhenting Wang, 2007. Impacts of wind velocity on sand and dust deposition during dust storm as inferred from a series of observations in the northeastern Qinghai–Tibetan Plateau, China. Powder Technology 175, 82-89.
5. Qiang Mingrui, Chen Fahu, Zhang Jiawu, Gao Shangyu, Zhou Aifeng, 2005. Climatic changes documented by stable isotopes of sedimentary carbonate in Lake Sugan, northeastern Tibetan Plateau of China, since 2 ka BP. Chinese Science Bulletin, 50(17), 1930-1939.
6. Qiang Ming-rui, Li Sen, Gao Shang-yu, 2004. Evidence for abrupt climatic changes on the northwestern margin of the East Asian monsoon during the last Deglaciation. Chinese Geographical Science 14(2), 117-121.
7.F. H. Chen, M. R. Qiang, Z. D. Feng et al., 2003. Stable East Asian monsoon climate during the last interglacial (Eemian) indicated by paleosol S1 in the western part of the Chinese Loess Plateau. Global and Planetary Change 36(3), 171-179.
8.Gao Shangyu, Lu Ruijie, Qiang Mingrui, et al. Reconstruction of precipitation in the last 140 years from tree ring at south margin of the Tengger Desert, China. Chinese Science Bulletin, 2005, 50(21): 2487-2492
9.Zhou AiFeng, Chen FaHu, Qiang MingRui, Yang MeiLin, Zhang JiaWu, 2007. The discovery of annually laminated sediments (varves) from shallow Sugan Lake in inland arid China and their paleoclimatic significance. Science in China (D Series) 50(8), 1218-1224.
10.Ruiping Zu, Xian Xue, Mingrui Qiang, Bao Yang, Jianjun Qu, Kecun Zhang, 2008. Characteristics of near-surface wind regimes in the Taklimakan Desert, China. Geomorphology 96, 39–47.