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姓 名:燕青
职 务
职 称:副研究员
研究方向:古冰盖、古台风和古东亚季风气候模拟研究
进所时间:0000-00-00
教育
2004--2008 兰州大学大气科学学院; 学士

2008--2013 中科院大气物理研究所;博士

2011--2012 挪威南森环境与遥感中心;交流学习

研究经历

任职经历
2013--2015 中科院大气物理研究所;助理研究员

2016--至今 中科院大气物理研究所;副研究员


研究项目
2018--2020,中国科协青年人才托举工程。

2018--2021,中上新世热带气旋特征及其气候反馈作用的模拟研究,面上基金。

2015--2017,晚上新世北半球冰盖形成过程中水汽输送加强的可能机制探究,青年基金。


重要著作

Accepted
Li Xiangyu, Zhang Ran, Zhang Zhongshi, Yan Qing, 2018: What enhanced the aridity in Eocene Asian inland: Global cooling or early Tibetan Plateau uplift? Palaeogeography, Palaeoclimatology, Palaeoecology, doi:10.1016/j.palaeo.2017.10.029
Li Xiangyu, Zhang Ran, Zhang Zhongshi, Yan Qing, 2018: Do climate simulations support the existence of East Asian monsoon climate in the Late Eocene? Palaeogeography, Palaeoclimatology, Palaeoecology, doi: 10.1016/j.palaeo.2017.12.037


2018
[37]. Shi Jian, Yan Qing*, Wang Huijun, 2018: Timescale-dependence of the relationship between the East Asian summer monsoon strength and precipitation over eastern China in the last millennium. Climate of the Past, 14, 577-591.
[36]. Yan Qing, Zhang Zhongshi, Wang Huijun, 2018: Divergent responses of tropical cyclone genesis factors to strong volcanic eruptions at different latitudes. Climate Dynamics, 50(5), 2121-2136.
[35]. Wei Ting, He Shengping, Yan Qing, Dong Wenjie, Wen Xiaohang, 2018: Decadal shift in west China autumn precipitation and its association with sea surface temperature. Journal of Geophysical Research-Atmospheres, 123, 835-847.


2017
[34]. Yan Qing, and Zhang Zhongshi, 2017: Dominating roles of ice sheets and insolation in variation of tropical cyclone genesis potential over the North Atlantic during the last 21,000 years. Geophysical Research Letters, 44, 10,624-10,632.
[33]. Yan Qing, Wei Ting, and Zhang Zhongshi, 2017: Variations in large-scale tropical cyclone genesis factors over the western North Pacific in the PMIP3 last millennium simulations, Climate Dynamics, 48(3-4): 957-970.
[32]. Shi Jian, Yan Qing*, Wang Huijun, Min Jinzhong, and Jiang Ying, 2017: Investigating dynamic mechanisms for synchronous variation of East Asian and Australian summer monsoons over the last millennium, Palaeogeography, Palaeoclimatology, Palaeoecology, 480, 70-79.
[31]. 燕青, 张仲石, 张冉, 李香钰, 2017: 过去千年北大西洋热带气旋生成潜势的模拟研究:基于PMIP3气候模式, 第四纪研究, 37(5): 1041~1050.
[30]. 张仲石, 燕青, 张冉, 李香钰, 戴高文, 冷姗, 田雨润, 2017: 第四纪北半球冰盖发育与东亚气候的遥相关, 第四纪研究, 37(5): 1009~1016.


2016
[29]. Yan Qing, Zhang Zhongshi, and Wang Huijun, 2016: Investigating uncertainty in the simulation of the Antarctic ice sheet during the mid-Piacenzian. Journal of Geophysical Research-Atmosphere, 121, 1559–1574.
[28]. Yan Qing, Wei Ting, Korty Robert, James Kossin, Zhang Zhongshi, and Wang Huijun, 2016: Enhanced intensity of global tropical cyclones during the mid-Pliocene warm period. Proceedings of the National Academy of Sciences, 113(46), 12963-12967.
[27]. Shi Jian, Yan Qing*, Jiang Dabang, Min Jingzhong and Jiang Ying, 2016: Precipitation variation over eastern China and arid central Asia during the past millennium and its possible mechanism: perspectives from PMIP3 experiments, Journal of Geophysical Research-Atmosphere, 121 (20), 11,989–12,004.
[26]. Zhou Xin, Sun Liguang, Zhan Tao, Huang Wen, Zhou Xinying, Hao Qingzhen, Wang Yuhong, He Xiaoqing, Zhao Chao, Zhang Jun, Qiao Yansong, Ge Junyi, Yan Pei, Yan Qing, Shao Da, Chu, Zhuding, Yang Wenqing, and Smol, John P, 2016: Time-transgressive onset of the Holocene Optimum in the East Asian monsoon region, Earth and Planetary Science Letters, 456, 39-46.
[25]. Zhang Ran, Zhang Zhongshi, Jiang Dabang, Yan Qing, Zhou Xin, and Cheng Z, 2016: Strengthened African Summer Monsoon in the Mid-Piacenzian. Advances in Atmospheric Sciences, 33 (9), 1061–1070.
[24]. Wei Ting, Dong Wenjie, Moore John, Song Yi, Yan Qing, Yang Zhiyong, Yuan Wenping, Chou Jieming, Cui Xuefeng, Yan,Xiaodong, Wei Zhigang, Guo, Yan, Yang Shili, Tian Di, Lin Pengfei, Yang Song, Wen Zhiping, Lin Hui, Chen Min, Feng Guolin, Jiang Yundi, Zhu Xian, Chen Juan, Wei Xin, Shi Wen, Zhang Zhiguo, Dong Juan, Li Yexin, Chen Deliang, 2016: Quantitative estimation of the climatic effects of carbon transferred by international trade, Scientific Reports, 6, DOI:10.1038/srep28046
[23]. Wei Ting, Dong Wenjie, Yan Qing, Chou Jieming, Yang Zhiyong, and Tian Di, 2016: Developed and developing world contributions to climate system change based on carbon dioxide, methane and nitrous oxide emissions. Advances in Atmospheric Sciences, 33(5), 632–643.
[22].张仲石,李香钰,燕青,张冉,2016:上新世海道变化对中国气候的影响,第四纪研究, 36(3), 768-774.


2015
[21]. Yan Qing, Korty Robert, and Zhang Zhongshi, 2015: Tropical cyclone genesis factors in a simulation of the last two millennia: Results from community earth system model. Journal of Climate, 28, 7182–7202.
[20]. Yan Qing, Zhang Zhongshi, Wang Huijun, and Jiang Dabang, 2015: Simulated warm periods of climate over China during the last two millennia: The Sui-Tang warm period versus the Song-Yuan warm period. Journal of Geophysical Research-Atmosphere, 120(6), 2229−2241.
[19]. Yan Qing, Zhang Zhongshi, and Wei Ting, 2015: Simulated spatio-temporal characteristics of climate change in China during the Han Dynasty (1−200 AD). Atmospheric and Oceanic Science Letters, 8, 352–357.
[18]. Gao Yongqi, Sun Jianqi, Li Fei, He Shengping, Sandven Stein, Yan Qing, Zhang Zhongshi, Lohmann Katja, Keenlyside Noel, Furevik Tore, and Suo Lingling, 2015: Arctic sea ice and eurasian climate: A review. Advances in Atmospheric Sciences, 32(1), 92−114.
[17]. Dolan AM, Hunter SJ, Hill DJ, Haywood AM, Koenig SJ, Otto-Bliesner BL, Abe-Ouchi A, Bragg F, Chan WL, Chandler MA, Contoux C, Jost A, Kamae Y, Lohmann G, Lunt DJ, Ramstein G, Rosenbloom NA, Sohl L, Stepanek C, Ueda H, Yan Qing, and Zhang Z, 2015: Using results from the PlioMIP ensemble to investigate the Greenland Ice Sheet during the mid-Pliocene Warm Period. Climate of the Past, 11(3), 203−424.
[16]. Li Xiangyu, Jiang Dabang, Zhang Zhongshi, Zhang Ran, Tian Zhiping, and Yan Qing, 2015: Mid-Pliocene westerlies from PlioMIP simulations. Advances in Atmospheric Sciences, 32(7), 900−923.
[15].魏婷,董文杰,武炳义,杨世莉,燕青,2015: 近期碳排放趋势对气候变化历史责任归因的影响,科学通报,7, 674-680.


2014
[14]. Yan Qing, Zhang Zhongshi, Wang Huijun, and Zhang Ran, 2014: Simulation of the Greenland Ice sheet during the mid-Pliocene. Chinese Science Bulletin, 59(2), 201−211, 2014.
[13]. Yan Qing, Wang Huijun, Johannessen Ola, and Zhang Zhongshi, 2014: Greenland ice sheet contribution to future global sea level rise based on CMIP5 models. Advances in Atmospheric Sciences, 31(1), 8−16.
[12]. Zhang Zhongshi, Ramstein Gilles, Schuster Mathieu, Li Camille, Contoux Camille and Yan Qing, 2014: Aridification of the Sahara desert caused by Tethys Sea shrinkage during the Late Miocene, Nature, 513(7518), 401−405.


2013
[11]. Yan Qing, Zhang Zhongshi, Gao Yongqi, Wang Huijun, and Johannessen Ola, 2013: Sensitivity of the modeled present-day Greenland Ice Sheet to climatic forcing and spin-up methods and its influence on future sea level projections, Journal of Geophysical Research-Earth Surface, 118(4), 2174−2189.
[10]. Zhang Ran, Yan Qing, Zhang Zhongshi, Jiang Dabang, Otto-Bliesner BL, Haywood, AM, Hill DJ, Dolan AM., Stepanek C, Lohmann G, Contoux C, Bragg F, Chan WL, Chandler MA, Jost A, Kamae Y, Abe-Ouchi A, Ramstein G, Rosenbloom NA, Sohl L, and Ueda H, 2013: Mid-Pliocene East Asian monsoon climate simulated in the PlioMIP. Climate of the Past, 9, 2085−2099.
[9]. Haywood AM, Hill DJ, Dolan AM, Otto-Bliesner BL, Bragg F, Chan WL, Chandler MA, Contoux C, Dowsett HJ, Jost A, Kamae Y, Lohmann G, Lunt DJ, Abe-Ouchi A, Pickering SJ, Ramstein G, Rosenbloom NA, Salzmann U, Sohl L, Stepanek C, Ueda H, Yan Qing, and Zhang Z, 2013: Large-scale features of Pliocene climate: results from the Pliocene Model Intercomparison Project. Climate of the Past, 9, 191−209.
[8]. Dowsett HJ, Foley KM, Stoll DK, Chandler MA, Sohl LE, Bentsen M, Otto-Bliesner BL, Bragg FJ, Chan WL, Contoux C, Dolan AM, Haywood AM, Jonas JA, Jost A, Kamae Y, Lohmann G, Lunt DJ, Nisancioglu KH, Abe-Ouchi A, Ramstein G, Riesselman CR, Robinson MM, Rosenbloom NA, Salzmann U, Stepanek C, Strother SL, Ueda H, Yan Qing, and Zhang Z, 2013: Sea surface temperature of the mid-Piacenzian ocean: A data-model comparison, Scientific Reports, 3. doi:10.1038/srep02013.


2012
[7]. Yan Qing, Zhang Zhongshi, Wang Huijun, Gao Yongqi, and Zheng Weipeng, 2012: Set-up and preliminary results of mid-Pliocene climate simulations with CAM3.1. Geoscientific Model Development, 5(2), 289−297.
[6]. Yan Qing, Zhang Zhongshi, and Gao Yongqi, 2012: An East Asian monsoon in the mid-Pliocene, Atmospheric and Oceanic Science Letters, 5(6), 449−454.
[5]. Zhang Zhongshi and Yan Qing, 2012: Pre-industrial and mid-Pliocene simulations with NorESM-L: AGCM simulations. Geoscientific Model Development, 5, 1033−1043.
[4]. Zhang Zhongshi, Yan Qing, Su Jingzhi, and Gao Yongqi, 2012: Has the problem of a permanent El Niño been resolved for the mid-Pliocene? Atmospheric and Oceanic Science Letters, 5, 445−448.
[3]. Zhang Zhongshi, Nisancioglu K, Bentsen M, Tjiputra J, Bethke I, Yan Qing, Risebrobakken B, Andersson C and Jansen E, 2012: Pre-industrial and mid-Pliocene simulations with NorESM-L. Geoscientific Model Development, 5, 523−533.


2011
[2]. Yan Qing, Zhang Zhongshi, Wang Huijun, Jiang Dabang and Zheng Weipeng, 2011: Simulation of sea surface temperature changes in the Middle Pliocene warm period and comparison with reconstructions. Chinese Science Bulletin, 56(9), 890−899.


2010
[1]. Zhang Zhongshi, Yan Qing, and Wang Huijun, 2010: Has the Drake Passage played an essential role in the Cenozoic cooling? Atmospheric and Oceanic Science Letters, 3, 288-292.

代表著作:

1) Q. Yan, Z. Zhang, H. Wang and D. Jiang, 2015: Simulated warm periods of climate over China during the last two millennia: The Sui-Tang warm period versus the Song-Yuan warm period. Journal of Geophysical Research, , <摘要>

当我们回顾中国的历史,唐朝的辉煌常让人津津乐道,宋朝的文弱常让人扼腕叹息。农业社会的中国,其实力的强弱往往和气候联系在一起;气候暖的时候,中国古代社会就会强盛。其实,唐朝和宋朝是我国过去两千年中两个典型的暖期,其温度与二十世纪早期相当。经济、教育、文化和外交在这两个朝代都取得了重要的进展。为什么类似的暖期气候条件会导致让人感觉截然不同的朝代,这是一个非常重要的自然和社会科学问题。利用耦合模式CESM,我们开展了过去两千年(0&minus;2000 AD)的瞬变模拟试验,比较了唐朝初期(650&minus;700 AD)和宋朝初期(950&minus;1000 AD)中国气候变化特征。研究发现尽管这两个时期,中国平均温度均偏高,但在空间分布上有很大的差异。唐朝初期增温主要出现在黄河流域、中原腹地,是区域尺度上大气净能量的增加以及有利的热量输送所造成的;而宋朝初期全国普遍增温,是太阳辐射强度的增加造成的。因此,唐朝暖期是一个区域现象,而宋朝暖期是全球或半球尺度上的暖事件在中国的体现。<br /> Qing Yan,&nbsp;Zhongshi Zhang,&nbsp;Huijun Wang and Dabang Jiang, 2015: Simulated warm periods of climate over China during the last two millennia: The Sui-Tang warm period versus the Song-Yuan warm period, Journal of Geophysical Research, doi: 10.1002/2014JD022941.<br /> 文章链接:<a href="http://onlinelibrary.wiley.com/doi/10.1002/2014JD022941/abstract">http://onlinelibrary.wiley.com/doi/10.1002/2014JD022941/abstract</a><br />
图1. 模拟的唐朝初期(650−700 AD; a)和宋朝初期(950−1000 AD; b)年平均温度的异常。 
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