李育(教授)


【来源:兰州大学资源环境学院 | 发布日期:2018-03-07 】     【选择字号:
姓名 李育 性别

最高学历 研究生 最高学位 博士
职务 科研副院长
职称

教授、博导

联系方式

Email:liyu@lzu.edu.cn

所在部门

地理系(硕/博研究生招生专业:地球系统科学)

研究方向

气候变化

学习经历

2000年-2004年,兰州大学,地理学基地班毕业获学士学位
2004年-2009年,兰州大学,地球系统科学专业毕业获理学博士学位

2008年-2009年,美国University of Colorado at Boulder和美国NOAA Paleo-climate Branch,中美联合培养博士研究生
工作经历

2010年-2011年,兰州大学,资源环境学院地球系统科学研究所任讲师
2012年,美国University of Colorado at Boulder和美国NOAA Paleo-climate Branch访问学者
2011年-2014,兰州大学,资源环境学院地球系统科学研究所任副教授、硕士生导师
2014年-今,兰州大学,资源环境学院地球系统科学研究所任教授、博士生导师
2016年,美国University of Utah访问学者

2017年,美国California Institute of Technology客座研究员
主讲课程

本科生课程(基地班):<气候学><自然地理野外综合实习>

研究生课程:<气候学><气候变化研究方法><学术论文写作-地球科学类><硕/博士研究生Seminar>
学术兼职

教育部高等学校地理科学类专业教学指导委员会常务副秘书长、国家自然科学基金委、国家留学基金委、甘肃省科技厅等多个学术部门评审;
、< Scientific Reports>、< JGR-Atmosphere>、等国际著名期刊通讯评议人;

中国地理学会会员、中国第四纪科学研究会会员、中国古生物学会孢粉学分会会员
研究成果

随着古气候学的发展,仅使用代用指标重建古气候变化已不能满足学科发展需要。李育研究组在古气候学研究中,以古气候模拟、古气候重建和现代气候观测相结合为研究思路,主要完成了以下三方面研究:

(1)在流域尺度上,以河西走廊内流河流域为例,在古环境记录基础上结合古气候模拟、古季风模拟、湖泊能量与水量平衡模拟,古降水量和古径流量定量重建等方法,系统地重建并模拟了全新世时期古气候与湖泊演化过程,并提出了河西走廊古水循环与无机碳汇模式,解决了该区域古气候学的定量化问题。研究结果显示,全新世时期石羊河流域终端湖的湖泊面积约628 km2,流域古降水量约为248.325~250.576 mm,中全新世无机碳汇速率约0.89 g C m-2 yr-1,植被碳汇速率约125g C m-2 yr-1,指示了中全新世气候适宜期。
该方向代表性论文:
[1] Li, Y., Xu, L., 2016. Asynchronous Holocene Asian monsoon vapor transport and precipitation. PalaeogeographyPalaeoclimatologyPalaeoecology 461, 195-200. (Impact factor: 2.578)
[2] Li, Y., Wang, N.A., Carrie, M., Anderson, D.M., Li, Z., Zhang, C., Zhou, X., 2012. Millennial-scale erosion rates in three inland drainage basins and their controlling factors since the Last Deglaciation, arid China. Palaeogeography, Palaeoclimatology, Palaeoecology 365–366, 263–275. (Impact factor: 2.578)
[3] Li, Y., Wang, N.A., Cheng, H., Long, H., Zhao, Q., 2009. Holocene environmental change in the marginal area of the Asian monsoon: a record from Zhuye Lake, NW China. Boreas 38, 349–361. (Impact factor: 2.386)
[4] Li, Y., Wang, N.A., Morrill, C., Cheng, H., Long, H., Zhao, Q., 2009. Environmental change implied by the relationship between pollen assemblages and grain-size in N.W. Chinese lake sediments since the Late Glacial. Review of Palaeobotany and Palynology 154, 54–64. (Impact factor: 2.158)
[5] Li, Y., Li, P., Zhang, C., Wang, Y. 2017. Long-Term Fine-Grained Sediment Records in a Drainage System in Arid China: A New Perspective from Paleo-Climatological Records and Simulations. Annals of the American Association of Geographers 107(5), 1216–1228. (Impact factor: 2.799)
[6] Li, Y., Zhang, C., Li, P., Wang, Y. 2017. Basin-Wide Sediment Grain-Size Numerical Analysis and Paleo-Climate Interpretation in the Shiyang River Drainage Basin. Geographical Analysis 49(3), 309–327 (Impact factor: 1.905)
[7] Li, Y., Wang, N., Li, Z., Zhang, H., 2011. Holocene palynological records and their responses to the controversies of climate system in the Shiyang River drainage basin. Chinese Science Bulletin 56, 535–546. (Impact factor: 2.275)
[8] Li, Y., Wang, N.A., Li, Z., Zhang, C., Zhou, X., 2012. Reworking effects in the Holocene Zhuye Lake sediments: A case study by pollen concentrates AMS 14C dating. Science China-Earth Sciences 55, 1669–1678. (Impact factor: 1.989)
[9] Li, Y., Wang, N., Li, Z., Zhou, X., Zhang, C., 2013. Climatic and environmental change in Yanchi Lake, Northwest China since the Late Glacial: A comprehensive analysis of lake sediments. Journal of Geographical Sciences 23, 932–946. (Impact factor: 2.364)
(2)在区域尺度上,将古气候模式与亚洲季风记录相结合,并提出了一个新的古气候模式与湖泊能量-水量平衡模型的耦合方法,系统性地模拟了东、中亚地区末次盛冰期和全新世古气候与湖泊演化过程,发现了东、中亚地区湖泊演化的不同步性,以及季风在不同时间尺度对暖期和海冰响应的差异,提出了夏季风与湖泊蒸发变化之间的反馈效应。
该方向代表性论文:
[1] Li, Y., Morrill, C., 2010. Multiple factors causing Holocene lake-level change in monsoonal and arid central Asia as identified by model experiments. Climate Dynamics 35, 1115–1128. (Impact factor: 4.708)

[2] Li, Y., Morrill, C., 2015. A Holocene East Asian winter monsoon record at the southern edge of the Gobi Desert and its comparison with a transient simulation. Climate Dynamics 45,1219–1234. (Impact factor: 4.708)
[3] Li, Y., Morrill, C., 2013. Lake levels in Asia at the Last Glacial Maximum as indicators of hydrologic sensitivity to greenhouse gas concentrations. Quaternary Science Reviews 60, 1–12. (Impact factor:4.797)
[4] Li, Y., Xu, L., Zhang, C., Liu, Y., Zhu, G., Zhou, X., 2018. Temporal and spatial evolution of Holocene vegetation and lake hydrological status, China. The Holocene, DOI: 10.1177/0959683617744260. (Impact factor: 2.324)
[5] Li, Y., Wang, N., Zhou, X., Zhang, C., Wang, Y., 2014. Synchronous or asynchronous Holocene Indian and East Asian summer monsoon evolution: a synthesis on Holocene Asian summer monsoon simulations, records and modern monsoon indices. Global and Planetary Change 116, 30–40. (Impact factor: 3.915)
[6] Li, Y., Zhang, C., Wang, Y., 2016. The verification of millennial-scale monsoon water vapor transport channel in northwest China. Journal of Hydrology, 536, 273-283. (Impact factor: 3.483)
[7] Li, Y., Wang, N.A., Chen, H., Li, Z., Zhou, X., Zhang, C., 2012. Tracking millennial-scale climate change by analysis of the modern summer precipitation in the marginal regions of the Asian monsoon. Journal of Asian Earth Sciences 58, 78–87. (Impact factor: 2.647)
(3)在全球尺度上,通过古气候记录与无机碳汇模型相结合的方法,提出内流河流域无机碳汇的“终端区域评价模式”,定量估算了全球内流河流域全新世无机碳汇速率与总量,解释了古气候变化与碳汇过程的关系,该研究对内流河流域水、碳循环机制以及未来全球变化研究具有重要意义。研究结果显示,中全新世时期全球内流河区域无机碳汇速率约为0.211 Pg C yr-1,高于现代的0.152 Pg C yr-1,无机碳汇总量相当于全球深海碳埋藏量。
该方向代表性论文:
[1] Li, Y., Zhang, C., Wang, N., Han, Q., Zhang, X., Liu, Y., Xu, L., Ye, W., 2017. Substantial inorganic carbon sink in closed drainage basins globally, Nature Geoscience, 10, 501-506. (Impact factor: 13.941)

[2] Li, Y., Liu, Y., Ye, W., Xu, L., Zhu, G., Zhang, X., Zhang, C., 2018. A new assessment of modern climate change, China—An approach based on paleo-climate, Earth-Science Reviews, 177, 458-477. (Impact factor: 7.051)

获得荣誉

 

在研项目

[1] 主持国家自然科学基金委面上项目:石羊河流域千年尺度垂直地带性规律与定量重建模型构建(No. 41571178)(国家级2016.1-2019.12)75万
[2] 主持国家自然科学基金委面上项目:风成沉积环境与水循环对流域性千年尺度气候变化的响应——以石羊河流域为例(No. 41371009)(国家级2014.1-2017.12)85万
[3] 主持国家自然科学基金委青年项目:猪野泽中全新世沉积地层与古湖泊岸堤对比研究(No. 41001116)国家级(2011.1-2013.12)25万
[4] 主持中央高校面上项目:季风边缘区全新世风成沉积物对气候变化的响应及模拟(lzujbky-2015-143)(2015.1- 2016.6)5万

[5] 主持中央高校面上项目:流域性风成与湖相沉积物对气候变化响应的差异性分析——以石羊河流域为例(lzujbky-2013-127)(2013.1- 2014.6)9万
[6] 主持中央高校面上项目:猪野泽沉积物孢粉浓缩物及炭屑AMS C测年(lzujbky-2010-99)(2010.7- 2012.6)6万
[7] 参与国家自然科学基金委项目:复杂环境下泾河流域汛期难控制利用洪水临界效应研究(No. 51109103)2012.1-2014.12

[8] 参与国家自然科学基金委项目:青海湖小冰期以来气候变化的生态水文效应(No. 40901021)2010.1-2012.12

发表论文

选取10篇代表性SCI论文:
[1] Li, Y., Zhang, C., Wang, N., Han, Q., Zhang, X., Liu, Y., Xu, L., Ye, W., 2017. Substantial inorganic carbon sink in closed drainage basins globally. Nature Geoscience, 10, 501-506. (Impact factor: 13.941)
[2] Li, Y., Liu, Y., Ye, W., Xu, L., Zhu, G., Zhang, X., Zhang, C., 2018. A new assessment of modern climate change, China—An approach based on paleo-climate. Earth-Science Reviews, 177, 458-477. (Impact factor: 7.051)
[3] Li, Y., Morrill, C., 2010. Multiple factors causing Holocene lake-level change in monsoonal and arid central Asia as identified by model experiments. Climate Dynamics 35, 1115–1128. (Impact factor: 4.708)
[4] Li, Y., Morrill, C., 2015. A Holocene East Asian winter monsoon record at the southern edge of the Gobi Desert and its comparison with a transient simulation. Climate Dynamics 45, 1219–1234. (Impact factor: 4.708)
[5] Li, Y., Morrill, C., 2013. Lake levels in Asia at the Last Glacial Maximum as indicators of hydrologic sensitivity to greenhouse gas concentrations. Quaternary Science Reviews 60, 1–12. (Impact factor:4.797)
[6] Li, Y., Xu, L., Zhang, C., Liu, Y., Zhu, G., Zhou, X., 2018. Temporal and spatial evolution of Holocene vegetation and lake hydrological status, China. The Holocene, DOI: 10.1177/0959683617744260. (Impact factor: 2.324)
[7] Li, Y., Wang, N., Zhou, X., Zhang, C., Wang, Y., 2014. Synchronous or asynchronous Holocene Indian and East Asian summer monsoon evolution: a synthesis on Holocene Asian summer monsoon simulations, records and modern monsoon indices. Global and Planetary Change 116, 30–40. (Impact factor: 3.915)

[8] Li, Y., Zhang, C., Wang, Y., 2016. The verification of millennial-scale monsoon water vapor transport channel in northwest China. Journal of Hydrology, 536, 273-283. (Impact factor: 3.483)
[9] Li, Y., Xu, L., 2016. Asynchronous Holocene Asian monsoon vapor transport and precipitation. PalaeogeographyPalaeoclimatologyPalaeoecology 461, 195-200. (Impact factor: 2.578)

[10] Li, Y., Wang, N.A., Carrie, M., Anderson, D.M., Li, Z., Zhang, C., Zhou, X., 2012. Millennial-scale erosion rates in three inland drainage basins and their controlling factors since the Last Deglaciation, arid China. Palaeogeography, Palaeoclimatology, Palaeoecology 365–366, 263–275. (Impact factor: 2.578)