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姓名:田芝平 (TIAN Zhiping)

职 称:副研究员/Associate Professor

研究方向: 古气候模拟,气候动力学/Paleoclimate Modeling, Climate Dynamics

邮箱tianzhiping@mail.iap.ac.cn

教育

2005/9–2009/7:成都信息工程学院,大气科学系,获理学学士学位
2009/9–2014/7:中国科学院大气物理研究所,气象学,获理学博士学位 

工作经历

2014/7–2018/3: 中国科学院大气物理研究所,助理研究员 
2015/12–2016/11: 美国夏威夷大学国际太平洋研究中心,访问学者
2018/3–至今: 中国科学院大气物理研究所,副研究员 


Email: tianzhiping@mail.iap.ac.cn

Education:

2005/9–2009/7, Bachelor, Department of Atmospheric Sciences, Chengdu University of Information Technology, China

2009/9–2014/7, Ph.D., Institute of Atmospheric Physics, Chinese Academy of Sciences, China

Research Experience:

2014/7–2018/3      Assistant Professor, Institute of Atmospheric Physics, Chinese Academy of Sciences, China

2015/12–2016/11  Visiting Scholar, International Pacific Research Center, University of Hawaii, USA

2018/3–                Associate Professor, Institute of Atmospheric Physics, Chinese Academy of Sciences, China


[1]     Jiang, D., X. Lang, Z. Tian, and D. Guo, 2011: Last glacial maximum climate over China from PMIP simulations. Palaeogeography, Palaeoclimatology, Palaeoecology, 309, 347−357.

[2]     Zhang, R., D. Jiang, X. Liu, and Z. Tian, 2012: Modeling the climate effects of different subregional uplifts within the Himalaya-Tibetan Plateau on Asian summer monsoon evolution. Chinese Science Bulletin, 57, 4617−4626.

[3]     田芝平,姜大膀,张冉,隋月, 2012: CCSM4.0的长期积分试验及其对东亚和中国气候模拟的评估. 大气科学, 36, 619−632.

[4]     Jiang, D., X. Lang, Z. Tian, and T. Wang, 2012: Considerable model-data mismatch in temperature over China during the mid-Holocene: Results of PMIP simulations. Journal of Climate, 25, 4135−4153.

[5]     张冉,姜大膀,田芝平, 2013: 中上新世是否存在“永久厄尔尼诺”状态——一个耦合模式结果. 第四纪研究, 33, 1130−1137.

[6]     Sui Y., D. Jiang, and Z. Tian, 2013: Latest update of the climatology and changes in the seasonal distribution of precipitation over China. Theoretical and Applied Climatology, 113, 599−610.

[7]     Jiang, D., X. Lang, Z. Tian, and L. Ju, 2013: Mid-Holocene East Asian summer monsoon strengthening: Insights from Paleoclimate Modeling Intercomparison Project (PMIP) simulations. Palaeogeography, Palaeoclimatology, Palaeoecology, 369, 422−429.

[8]     田芝平,姜大膀, 2013: 不同分辨率CCSM4对东亚和中国气候模拟能力分析. 大气科学, 37, 171−186, doi:10.3878/j.issn.1006-9895.2012.12050.

[9]     Jiang, D., and Z. Tian, 2013: East Asian monsoon change for the 21st century: Results of CMIP3 and CMIP5 models. Chinese Science Bulletin, 58, 1427−1435.

[10]   Jiang, D., Z. Tian, and X. Lang, 2013: Mid-Holocene net precipitation changes over China: Model-data comparison. Quaternary Science Reviews, 82, 102−120.

[11]   Tian, Z., and D. Jiang, 2013: Mid-Holocene ocean and vegetation feedbacks over East Asia. Climate of the Past, 9, 2153−2171, doi:10.5194/cp-9-2153-2013.

[12]   Tian, Z., and D. Jiang, 2015: Mid-Holocene ocean feedback on global monsoon area and precipitation. Atmospheric and Oceanic Science Letters, 8, 29−32, doi:10.3878/AOSL20140068.

[13]   田芝平,姜大膀, 2015: 全新世中期和末次冰盛期中国季风区面积和季风降水变化. 科学通报, 60, 400−410, doi:10.1360/N972014-00718.

[14]   Li, X., D. Jiang, Z. Zhang, R. Zhang, Z. Tian, and Q. Yan, 2015: Mid-Pliocene westerlies from PlioMIP simulations. Advances in Atmospheric Sciences, 32, 909−923, doi:10.1007/s00376-014-4171-7.

[15]   Jiang, D., Z. Tian, and X. Lang, 2015: Mid-Holocene global monsoon area and precipitation from PMIP simulations. Climate Dynamics, 44, 2493−2512, doi:10.1007/s00382-014-2175-8.

[16]   Jiang, D., Z. Tian, X. Lang, M. Kageyama, and G. Ramstein, 2015: The concept of global monsoon applied to the last glacial maximum: A multi-model analysis. Quaternary Science Reviews, 126, 126−139.

[17]   Tian, Z., and D. Jiang, 2015: Revisiting mid-Holocene temperature over China using PMIP3 simulations. Atmospheric and Oceanic Science Letters, 8, 358−364, doi:10.3878/AOSL20150040.

[18]   Jiang, D., Z. Tian, and X. Lang, 2016: Reliability of climate models for China through the IPCC Third to Fifth Assessment Reports. International Journal of Climatology, 36(3), 1114−1133, doi:10.1002/joc.4406.

[19]   Tian, Z., and D. Jiang, 2016: Revisiting last glacial maximum climate over China and East Asian monsoon using PMIP3 simulations. Palaeogeography, Palaeoclimatology, Palaeoecology, 453, 115−126, doi:10.1016/j.palaeo.2016.04.020.

[20]   Tian, Z., T. Li, D. Jiang, and L. Chen, 2017: Causes of ENSO weakening during the mid-Holocene. Journal of Climate, 30(17), 7049−7070, doi:10.1175/JCLI-D-16-0899.1.

[21]   姜大膀, 田芝平, 2017: 末次冰盛期和全新世中期东亚地区水汽输送的模拟研究. 第四纪研究, 37(5), 999−1008, doi:10.11928/j.issn.1001-7410.2017.05.07.

[22]   Tian, Z., T. Li, and D. Jiang, 2018: Strengthening and westward shift of the tropical Pacific Walker circulation during the mid-Holocene: PMIP simulation results. Journal of Climate, 31(6), 2283−2298, doi:10.1175/JCLI-D-16-0744.1.

[23]   Tian, Z., and D. Jiang, 2018: Strengthening of the East Asian winter monsoon during the mid-Holocene. The Holocene, 28(9), 1443−1451, doi:10.1177/0959683618777076.

[24]   Xiao, J., S. Zhang, J. Fan, R. Wen, D. Zhai, Z. Tian, and D. Jiang, 2018: The 4.2 ka BP event: multi-proxy records from a closed lake in the northern margin of the East Asian summer monsoon. Climate of the Past, 14, 1417−1425, doi:10.5194/cp-14-1417-2018.

[25]   Jiang, D., Y. Sui, X. Lang, and Z. Tian, 2018: Last glacial maximum and mid-Holocene thermal growing season simulations. Journal of Geophysical Research: Atmospheres, 123(20), 11466−11478, doi:10.1029/2018JD028605.

[26]   苏宝煌, 姜大膀, 田芝平, 2018: 全球山脉隆升影响副热带干旱气候的模拟. 科学通报, 63(12), 1142−1153, doi:10.1360/N972017-01275.

[27]   Li, X., D. Jiang, Z. Tian, and Y. Yang, 2018: Mid-Pliocene global land monsoon from PlioMIP1 simulations. Palaeogeography, Palaeoclimatology, Palaeoecology, 512, 56−70, doi:10.1016/j.palaeo.2018.06.027.  

[28]   Tian, Z., and D. Jiang, 2020: Weakening and eastward shift of the tropical Pacific Walker circulation during the Last Glacial Maximum. Boreas, 49(1), 200−210, doi:10.1111/bor.12417.

[29]   Jiang, D., D. Hu, Z. Tian, and X. Lang, 2020: Differences between CMIP6 and CMIP5 models in simulating climate over China and the East Asian monsoon. Advances in Atmospheric Sciences, 37, 1102–1118, doi:10.1007/s00376-020-2034-y.

[30]   Chen, W., D. Jiang, X. Lang, and Z. Tian, 2021: Understanding the cold biases of CMIP5 models over China with weather regimes. Advances in Climate Change Research, 12(3), 373–383, doi:10.1016/j.accre.2021.05.002.

[31]   姜大膀, 田芝平, 王娜, 张冉, 2022: 末次冰盛期和中全新世气候模拟分析进展. 地球科学进展, 37(1), 113, doi:10.11867/j.issn.1001-8166.2021.098.

[32]   Tian, Z., D. Hu, X. Lang, and D. Jiang, 2022: Index- and model-dependent projections of East Asian summer monsoon in Coupled Model Intercomparison Project Phase 6 simulations. International Journal of Climatology, 42(4), 2208–2224, doi:10.1002/joc.7361. 

[33]   Hu, D., D. Jiang, Z. Tian, and X. Lang, 2022: How skillful was the projected temperature over China during 2002–2018? Science Bulletin, 67(10), 1077–1085, doi:10.1016/j.scib.2022.02.004.

[34]   Tian, Z., D. Jiang, R. Zhang, and B. Su, 2022: Transient climate simulations of the Holocene (version 1) – experimental design and boundary conditions. Geoscientific Model Development, 15(11), 4469–4487, doi:10.5194/gmd-15-4469-2022.

[35]   Shi, J., D. Jiang, Z. Tian, and X. Lang, 2022: Enhanced interannual variability in temperature during the Last Glacial Maximum. Journal of Climate, 35(18), 5933–5950, doi:10.1175/JCLI-D-21-0739.1.

[36]   田芝平, 张冉, 姜大膀, 2022: 全新世中期中国气候和东亚季风:PMIP4模式结果. 地学前缘, 29(5), 355371, doi:10.13745/j.esf.sf.2021.9.52.

[37]   Hu, D., D. Jiang, Z. Tian, and X. Lang, 2022: Weakened amplitude and delayed phase of the future temperature seasonal cycle over China during the twenty‐first century. International Journal of Climatology, 42(14), 7133–7145, doi:10.1002/joc.7634.

[38]   Chen, W., D. Jiang, X. Lang, and Z. Tian, 2022: Improved skill of Coupled Model Intercomparison Project phase 6 over phase 5 models in reproducing weather regimes in East Asia. International Journal of Climatology, 42(16), 92719287, doi:10.1002/joc.7817.

[39]   Hu, D., Z. Tian, X. Lang, and D. Jiang, 2023: Limited skill of projected land precipitation by IPCC models during 2002−2020. Journal of Geophysical Research: Atmospheres, 128(2), e2022JD037851, doi:10.1029/2022JD037851

[40]   Shi, J., Z. Tian, X. Lang, and D. Jiang, 2023: Past to future drylands in China: A multimodel analysis using CMIP6 simulations. Journal of Climate, 36(8), 2735–2751, doi:10.1175/JCLI-D-22-0720.1.

[41]   Jiang, Z.,  C. M. Brierley, J. Bader, P. Braconnot, M. Erb, P. O. Hopcroft, D. Jiang, J. Jungclaus, V. Khon, G. lohmann, O. Marti, M. B. Osman, B. Otto-Bliesner, B. Schneider, X. Shi, D. J. R. Thornalley, Z. Tian, and Q. Zhang, 2023: No consistent simulated trends in the Atlantic Meridional Overturning Circulation for the past 6,000 years. Geophysical Research Letters, 50(10), e2023GL103078, doi:10.1029/2023GL103078.

[42]   Yu, L., D. Si, D. Jiang, Y. Ding, X. Shen, X. Lang, Q. Li, and Z. Tian, 2023: Tibetan Plateau booster effect on the influence of Atlantic multidecadal variability on the East Asian summer rainfall. Journal of Climate, 36(10), 3437–3452, doi:10.1175/JCLI-D-22-0472.1.

[43]   Tian, Z., and D. Jiang, 2023: Enhanced seasonality of surface air temperature over China during the mid-Holocene. Atmospheric and Oceanic Science Letters, 16(5), 100393, doi:10.1016/j.aosl.2023.100393.

[44]   Yao, S., X. Lang, D. Si, and Z. Tian, 2023: Moisture sources of summer heavy precipitation in two spatial patterns over Northeast China during 1979–2021. Atmospheric Science Letters, 24(11), e1181, doi:10.1002/asl.1181.

[45]   Hu, D., Z. Tian, X. Lang, and D. Jiang, 2023: Regional difference in precipitation seasonality over China from CMIP6 projections. International Journal of Climatology, 43(13), 6179–6190, doi:10.1002/joc.8199.

[46]   Zhang, R., D. Jiang, S. Liu, C. Zhang, Z. Zhang, X. Li, Z. Tian, and J. Shi, 2024: Less dryland aridity during Pliocene warmth. Journal of Geophysical Research: Atmospheres, 129(2), e2023JD039371, doi:10.1029/2023JD039371.

[47]   Shi, J., Z. Tian, X. Lang, and D. Jiang, 2024: Projected changes in the interannual variability of surface air temperature using CMIP6 simulations. Climate Dynamics, 62(1), 431–446, doi:10.1007/s00382-023-06923-3.


 









现主持、参加项目:

[1] 国家自然科学基金面上项目“过去千年主要年代际气候模态对中国气候遥相关影响的模拟分析”(项目批准号:42375053,2024.01-2027.12),主持人

[2] 中国科学院青年创新促进会(2022.01-2025.12), 主持人

[3] 国家自然科学基金面上项目“全新世中国温度、降水年际和年代际变率的模拟分析与机制研究”(项目批准号:42075048,2021.01-2024.12),主持人

[4] 国家自然科学基金重点项目“全新世金钉子型气候突变事件:我国季风区湖泊记录”(项目批准号:41931181,2020.01-2024.12),项目骨干

曾主持、参加项目:

[1] 国家重点研发计划课题““一带一路”主要国家气候变化特征及风险研究”(2018.05-2023.04),项目骨干
[2] 中国科学院战略性先导科技专项“泛第三极环境变化与绿色丝绸之路建设”,子课题名称“西风季风变化模拟”(2018.03-2023.02),项目骨干

[3] 国家自然科学基金青年科学基金项目末次冰盛期和全新世中期欧亚西风带变化的模拟分析与机制研究项目批准号:41705064,2018.01-2020.12),主持人

[4] 国家重点研发计划课题“季风变异和干旱演变的驱动机制”(2017.07-2022.06),参加人

[5] 国家自然科学基金面上项目过去和未来全球变暖情景下气候—植被反馈作用的模拟研究(项目批准号:41175072,2012.01-2015.12),参加人