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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
青年科学基金“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(2015-2017)”

重要著作

Acceptted/In press
Yan Q., Zhongshi Zhang, and Huijun Wang (2017), Divergent responses of tropical cyclone genesis factors to strong volcanic eruptions at different latitudes, Clim. Dyn., doi: 10.1007/s00382-017-3739-1

2017
Shi J., Yan Q.*, Wang H., Min J., and Jiang Y. (2017), Investigating dynamic mechanisms for synchronous variation of East Asian and Australian summer monsoons over the last millennium, Palaeogeography, Palaeoclimatology, Palaeoecology, 480, 70-79.

Yan Q., T. Wei, and Z. Zhang (2017), Variations in large-scale tropical cyclone genesis factors over the western North Pacific in the PMIP3 last millennium simulations, Clim. Dyn, 48:957-970

2016
Yan Q., T. Wei, R. Korty, J. P. Kossin, Z. Zhang, and H. J. Wang, 2016: Enhanced intensity of global tropical cyclones during the mid-Pliocene warm period. Proc. Nat. Acad. Sci.,113, 12963–12967.

Shi, J.,Yan Q.*, D. Jiang, J. Min, and Y. Jiang (2016), Precipitation variation over eastern China and arid central Asia during the past millennium and its possible mechanism: perspectives from PMIP3 experiments, J. Geophys. Res. Atmos., 121,11,989–12,004, DOI:10.1002/2016JD025126

Zhou, X., Sun, L., Zhan, T., Huang, W., Zhou, X., Hao, Q., Wang, Y., He, X., Zhao, C., Zhang, J., Qiao, Y., Ge, J., Yan, P., Yan Q., Shao, D., Chu, Z., Yang, W., Smol, J.P., 2016. Time-transgressive onset of the Holocene Optimum in the East Asian monsoon region. Earth and Planetary Science Letters 456, 39-46.

Zhang R., Zhang Z., Jiang D., Yan Q., Zhou X., and Cheng Z .(2016), Strengthened African Summer Monsoon in the Mid-Piacenzian. Adv. Atmos. Sci., 33, 1061–1070.

Wei T., Dong W., Moore J., Yan Q., et al. (2016), Quantitative Estimation of the Climatic Effects of Carbon Transferred by International Trade. Scientific Reports, 6, DOI:10.1038/srep28046

Yan Q., Z. Zhang, and H. Wang (2016), Investigating uncertainty in the simulation of the Antarctic ice sheet during the mid-Piacenzian, J. Geophys. Res. Atmos., 121, 1559–1574, doi:10.1002/2015JD023900.

Wei, T., W. J. Dong, Yan Q., J. M. Chou, Z. Y. Yang, and D. Tian, 2016: Developed and developing world contributions to climate system change based on carbon dioxide, methane and nitrous oxide emissions. Adv. Atmos. Sci.,33(5), 632–643.

2015
Yan Q., Z. Zhang, and T. Wei: Simulated Spatiotemporal Characteristics of Climate Change in China during the Han Dynasty (1–200 A.D.). Atmos. Oceanic Sci. Lett., 8(6), 352-357, 2015.

Yan Q., R. Korty, and Z. Zhang:Tropical cyclone genesis factors in a simulation of the last two millennia: Results from community earth system model, Journal of Climate, 28, 7182–7202, 2015

Yan Q., Z. Zhang, H. Wang and D. Jiang, Simulated warm periods of climate over China during the last two millennia: The Sui-Tang warm period versus the Song-Yuan warm period, J. Geophys. Res.,120, 2229–2241, 2015.

Dolan, A. M., Hunter, S. J., Hill, D. J., Haywood, A. M., Koenig, S. J., Otto-Bliesner, B. L., Abe-Ouchi, A., Bragg, F., Chan, W.-L., Chandler, M. A., Contoux, C., Jost, A., Kamae, Y., Lohmann, G., Lunt, D. J., Ramstein, G., Rosenbloom, N. A., Sohl, L., Stepanek, C., Ueda, H., Yan Q., and Zhang, Z.: Using results from the PlioMIP ensemble to investigate the Greenland Ice Sheet during the mid-Pliocene Warm Period, Clim. Past, 11, 403-424, doi:10.5194/cp-11-403-2015, 2015.

Li X., Jiang D., Zhang Z., Zhang R, Tian Z., and Yan Q. , Mid-Pliocene Westerlies from PlioMIP Simulations. Adv. Atmos. Sci.,32,909-923,2015

Gao, Y.Q.,Sun J.Q.,Li F.,He S.P.,Sandven S., Yan Q., Zhang Z.S.,Lohmann K.,KEENLYSIDE N.,FUREVIK T.,and Suo L.L., Arctic Sea Ice and Eurasian Climate: A Review. Adv. Atmos. Sci., 32(1),92-114, 2015.

2014
Zhang, Z., Ramstein, G., Schuster, M., Li, C., Contoux, C., and Q.Yan, Aridification of the Sahara desert caused by Tethys Sea shrinkage during the Late Miocene, Nature, 513(7518), 401-404, 2014

Yan Q., H. J. Wang, O. M. Johannessen, and Z. S. Zhang, Greenland ice sheet contribution to future global sea level rise based on CMIP5 models, Adv. Atmos. Sci., 31, 8-16, 2014.

Yan Q., Z. Zhang, H. Wang and R. Zhang, Simulation of the Greenland Ice sheet during the mid-Pliocene, Chin. Sci. Bull., 59, 201-211, 2014.

2013
Yan Q., Z. Zhang, Y. Gao, H. Wang, and O. M. Johannessen, Sensitivity of the modeled present-day Greenland Ice Sheet to climatic forcing and spin-up methods and its influence on future sea level projections, J. Geophys. Res. Earth Surf., 118, 2174-2189, 2013

Zhang, R., Q.Yan, Z. S. Zhang, D. Jiang, B. L. Otto-Bliesner, A. M. Haywood, D. J. Hill, A. M. Dolan, C. Stepanek, G. Lohmann, C. Contoux, F. Bragg, W.-L. Chan, M. A. Chandler, A. Jost, Y. Kamae, A. Abe-Ouchi, G. Ramstein, N. A. Rosenbloom, L. Sohl, and H. Ueda, Mid-Pliocene East Asian monsoon climate simulated in the PlioMIP, Clim. Past, 9, 2085-2099, 2013.

Haywood, A. M., Hill, D. J., Dolan, A. M., Otto-Bliesner, B. L., Bragg, F., Chan, W. L., Chandler, M. A., Contoux, C., Dowsett, H. J., Jost, A., Kamae, Y., Lohmann, G., Lunt, D. J., Abe-Ouchi, A., Pickering, S. J., Ramstein, G., Rosenbloom, N. A., Salzmann, U., Sohl, L., Stepanek, C., Ueda, H., Yan Q. and Zhang, Z, Large-scale features of Pliocene climate: results from the Pliocene Model Intercomparison Project , Clim. Past, 9, 191-209, 2013

Dowsett, H. J., K. M. Foley, D. K. Stoll, M. A. Chandler, L. E. Sohl, M. Bentsen, B. L. Otto-Bliesner, F. J. Bragg, W.-L. Chan, C. Contoux, A. M. Dolan, A. M. Haywood, J. A. Jonas, A. Jost, Y. Kamae, G. Lohmann, D. J. Lunt, K. H. Nisancioglu, A. Abe-Ouchi, G. Ramstein, C. R. Riesselman, M. M. Robinson, N. A. Rosenbloom, U. Salzmann, C. Stepanek, S. L. Strother, H. Ueda, Q.Yan and Z. Zhang, Sea Surface Temperature of the mid-Piacenzian Ocean: A Data-Model Comparison, Sci. Rep., 3, 2013

2012
Yan Q., Z. Zhang, and Y. Gao, An East Asian Monsoon in the Mid-Pliocene, Atmos. Oceanic Sci. Lett, 5, 449-454, 2012.

Yan Q., Z. Zhang, H. Wang, Y. Gao, and W. Zheng, Set-up and preliminary results of mid-Pliocene climate simulations with CAM3.1, Geosci. Model Dev., 5, 289−297, 2012.

Zhang Z., and Q.Yan, Pre-industrial and mid-Pliocene simulations with NorESM-L: AGCM simulations, Geosci. Model Dev., 5, 1033-1043, 2012.

Zhang Z., Q.Yan, J. Su, and Y. Gao, Has the problem of a permanent El Niño been resolved for the Mid-Pliocene?, Atmos. Oceanic Sci. Lett, 5, 445-448, 2012.

Zhang, Z. S., Nisancioglu, K., Bentsen, M., Tjiputra, J., Bethke, I., Yan Q., Risebrobakken, B., Andersson, C., and Jansen, E.: Pre-industrial and mid-Pliocene simulations with NorESM-L, Geosci. Model Dev., 5, 523-533, doi:10.5194/gmd-5-523-2012, 2012.

2011
Yan Q., Z. Zhang, H. Wang, D. Jiang and W. Zheng, Simulation of sea surface temperature changes in the Middle Pliocene warm period and comparison with reconstructions, Chin. Sci. Bull., 56, 890−899, 2011.

2010
Zhang Z., Q.Yan, and H. Wang, Has the Drake Passage played an essential role in the Cenozoic cooling?, Atmos. Oceanic Sci. Lett., 3, 288-292, 2010.

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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