[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), 1−13, 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), 355−371, 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), 9271–9287, 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.

[48]   Tian, Z., 2024: Revisiting East Asian monsoon change during the Last Glacial Maximum using PMIP4 simulations. Atmospheric and Oceanic Science Letters, 17(3), 100467, doi:10.1016/j.aosl.2024.100467.

[49]   Wang, T., Z. Tian, and D. Jiang, 2024: Changes in the Asian ITCZ during the Last Interglacial, the Last Glacial Maximum, and the mid-Holocene. Journal of Geophysical Research: Atmospheres, 129(16), e2023JD040212, doi:10.1029/2023JD040212.

[50]   田芝平, 史嘉文, 姜大膀, 2024: 末次间冰期中国季风降水的模拟分析. 第四纪研究, 44(5), 1388–1398, doi:10.11928/j.issn.1001-7410.2024.05.24.

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