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个人简介

工作经历 2019-至今 南京师范大学地理科学学院 教授 南京师范大学地理科学学院地理信息科学系 副主任 2015-2019 南京师范大学地理科学学院 副教授 南京师范大学地理科学学院地理信息科学系 副主任 2018-至今 美国马萨诸塞大学地球科学系 兼职副教授 2015-2018 美国马萨诸塞大学地球科学系 兼职助理教授 2012-2015 美国马萨诸塞大学地球科学系,气候系统研究中心 美国内政部东北气候科学中心 博士后 合作导师: Dr. Raymond S. Bradley 教育背景 2012 美国宾夕法尼亚州立大学气象系 气象学博士 导师: Dr. Michael E. Mann 答辩委员会: Dr. Robert Crane, Dr. Raymond G. Najjar Jr., and Dr.Thorsten Wegener 2007 南京大学大气科学系 气象学硕士 导师: 钱永甫教授 2004 南京大学大气科学系 大气科学学士 导师: 钱永甫教授

研究领域

气候变率;气候变化;气候模拟;古气候;气候统计方法;气候降尺度;气候变化在水文、生态、环境研究中的应用

近期论文

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Ning, L., J. Liu, R. S. Bradley, M. Yan, K. Chen, W. Sun, and C. Jin, 2019:Elevation-dependent cooling caused by volcanic eruptions during last millennium. Int. J.Climatology, DOI: 10.1002/joc.6387 (online). Sun, W., B. Wang, Q. Zhang, F. S. R. Pausata, D. Chen, G. Lv, M. Yan, L. Ning, and L. Liu,2019: Northern Hemisphere land monsoon precipitation increased by the green Sahara during middle Holocene. Geophys. Res. Lett., 46, 9870-9879, doi: 10.1029/2019GL082116 Jin, C., L. Liu, B. Wang, L. Ning, and M. Yan, 2019: Decadal variability of northern Asian winter monsoon shaped by the 11-year solar Cycle. Clim. Dyn., 53, 6559-6568, DOI 10.1007/s00382-019-04945-4 Jin, C., L. Liu, B. Wang, M. Yan, and L. Ning, 2019: Decadal Variations of the East Asian Summer Monsoon Forced by the 11-Year Insolation Cycle. J. Climate, 32(10), 1735-1745. Sun, W., B. Wang, J. Liu, D. Chen, C. Gao, L. Ning, and L. Chen, 2019: How northern high-latitude volcanic eruptions in different seasons affect ENSO? J. Climate, 32,3245-3262. Sun, W., J. Liu, B. Wang, D. Chen, F. Liu, Z. Wang, L. Ning, and M Chen, 2019: A “La Niña-like” state occurring in the second year after large tropical volcanic eruptions during the past 1500 years. Clim. Dyn., 52(12), 7494-9509, doi:10.1007/s00382-018-4163-x Ning, L., J. Liu, B. Wang, K. Chen, M. Yan, C. Jin, and Q. Wang, 2019: Variability and mechanisms of megadroughts over eastern China during the last millennium: A model study.Atmosphere, 10, 7, doi:10.3390/atmos10010007. Ning, L., J. Liu, R. S. Bradley, and M. Yan, 2019: Comparing the spatial patterns of climate change in the 9th and 5th millennia B.P. from TRACE-21 model simulations. Climate of the Past, 15, 41-52, doi:10.5194/cp-15-41-2019 Liu, L., T. Zhou, L. Ning*, J. Liu, M. Yan, C. Jin, and W. Sun, 2019: Linkage between the Arctic Oscillation and summer climate extreme events over the middle reaches of Yangtze River Valley. Climate Research, 78, 237-247, doi: 10.3554/cr01542 Liu, L., L. Ning*, J. Liu, M. Yan, and W. Sun 2019: Prediction of Summer Extreme Precipitation over the Middle and Lower Reaches of the Yangtze River Basin, Int. J.Climatology, 39, 375-383, doi: 10.1002/joc.5813 Yan, M., B. Wang, J. Liu, A. Zhu, L. Ning, and J. Cao, 2018: Understanding the Australian Monsoon change during the Last Glacial Maximum with a multi-model ensemble. Climate of the Past, 14, 2037-2052, doi:10.5194/cp-14-2047-2018 Sinha, P., M. E. Mann, J. D. Fuentes, A. Mejia, L. Ning, W. Sun, T. He, and J. Obeysekera,2018: Downscaled rainfall projections in south Florida using self-organizing maps. Science of the Total Environment, 635, 1110-1123. Ning, L., J. Liu, Z. Wang, and R. S. Bradley, 2018: Different influences on the tropical Pacific SST gradient from natural forcing and anthropogenic forcing. Int. J. Climatology, 38,2015-2028, doi:10.1002/joc.5313. Ning, L., J. Liu, and B. Wang, 2017: How does South Asian High influence extreme precipitation over eastern China? J. Geophys. Res. Atmos., 122, 4281-4298, doi:10.1002/2016JD026075 Ning, L., J. Liu, and W. Sun, 2017: Influences of volcano eruptions on Asian Summer Monsoon over the last 110 years. Scientific Reports, 7, 42626, doi:10.1038/srep42626 Ning, L., and R. S. Bradley, 2016: NAO and PNA influences on winter temperature and precipitation over the eastern United States in CMIP5 GCMs. Clim. Dyn., 46(3),1257-1276, DOI: 10.1007/s00382-015-2643-9 Ning, L., and R. S. Bradley, 2015: Snow occurrence changes over the central and eastern United States under future warming scenarios. Scientific Reports, 5, 17073, doi:10.1038/srep17073

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