王美蓉

个人信息Personal Information

副教授硕士生导师

教师拼音名称：wangmeirong

所在单位：大气科学学院

办公地点：气象楼611

性别：女

职称：副教授

硕士生导师

学科：气象学

其他联系方式Other Contact Information

邮箱 : wmr@nuist.edu.cn

同专业硕导

基本信息
个人简介
近期主要论著
近期科研项目

姓       名:  王美蓉
出生年月:  1987年
国       籍:  中国
性       别:  女
导       师:  段安民研究员（硕博）、周顺武教授（硕）
职       称: 副教授
最高学历:  博士
所属专业:  气象学
所属系部:  动力气象系
毕业院校:  中国科学院大气物理研究所
研究方向:  青藏高原气象学
办公地点:  气象楼611室
邮       箱:  wmr@nuist.edu.cn
主讲课程:  动力气象学、高等动力气象学、天气系统动力学（雷丁学院）、气象统计方法、大气科学概论
主要研究领域:  青藏高原气候动力学、季节内振荡、东亚夏季风及中国降水、陆地植被年际变率

欢迎前往Researchgate下载原文：https://www.researchgate.net/profile/Meirong-Wang-2/research

2024

1、Zhu, Z., Wang, M. R.*, Wang, J., Duan, A. M., Liu, B. Q., and Yu, Z. S. Intraseasonal oscillation intensity variations of the atmospheric heat source over the Tibetan Plateau and their relationship with summer precipitation. Journal of Climate, 2024, accepted.

2、Tan, J. Y., Wang, J.*, Mao, H. Q., Wang, H. M., Liu, Z. Q., Wang, M. R., et al. Impact of net-zero emissions on atmospheric CO2 concentration in China: ideal simulations based on the GEOS-Chem model. Science China Earth Science. 2024, accepted.

3、Tan, J. Y., Wang, J.*, Wang, H. K., Liu, Z., Zeng, N., Yan, R., Dou, X. Y., Wang, X. M., Wang, M. R., et al., Influence of extreme 2022 heatwave on megacities’ anthropogenic CO2 emissions in lower-middle reaches of the Yangtze River. Science of the Total Environment. 2024, 951, 175605.

4、Yan, R., Wang, J*., Ju, W. M., Xing, X. L., Yu, M., Wang, M. R., et al. Distinct impacts of the El Nino-Southern Oscillation and Indian Ocean Dipole on China’s gross primary production. Biogeosciences. 2024, 21, 5027–5043.

2023

1、Wang, M.; Yao, X.*; Wang, J.; Liu, B.; Zhu, Z.; Zhou, S.; Yuan, J. (2023). Spatial Heterogeneity of Summer Rainfall Trends over the Tibetan Plateau Contributed by Different Rainfall Intensities. Remote Sens. 15, 5587. https://doi.org/10.3390/rs15235587

2、J Wang*, R Yan, G X Wu, Y M Liu, M R Wang, et al. (2023). Unprecedented decline in photosynthesis caused by summer 2022 record-breaking compound drought-heatwave over Yangtze River Basin. Science Bulletin, 68(19): 2160-2163. https://doi.org/10.1016/j.scib.2023.08.011

3、Z R Deng, S W Zhou*, M R Wang, et al. (2023). Variations in summer air temperature over the Eastern Tibetan Plateau: connection with Barents-Kara spring sea ice and summer Arctic Oscillation. Journal of Geophysical Research: Atmospheres, 128(21): https://doi.org/10.1029/2023JD039765

4、Z R Deng, S W Zhou*, M R Wang, et al. (2023). Changes in the midsummer extreme high-temperature events over the Yangtze River Valley associated with the thermal effect of the Tibetan Plateau and Arctic Oscillation. Atmospheric Research, 293(668): 106911.

5、周庶，孙芳，王美蓉*，周顺武，青逸雨，2023. 青藏高原热源对高原低涡不同发展阶段的影响——2013年7月个例分析. 大气科学，47(3): 907−919.

6、Wang, J.*, Zeng, N., Wang, M., Jiang, F., Chevallier, F., Crowell, S., et al. (2023). Anomalous net biome exchange over Amazonian rainforests induced by the 2015/16 El Niño: Soil dryness-shaped spatial pattern but temperature-dominated total flux. Geophysical Research Letters, 50, e2023GL103379. https://doi. org/10.1029/2023GL103379

7、Yang Sun, Sing Shan, Shunwu Zhou, Meirong Wang, et al, 2023. Corrigendum: Impacts of Tibetan Plateau sensible heat and El Nino-Southern Oscillation on precipitation over South China under the background of the PDO. Frontiers in Environmental Science, DOI:10.3389/fenvs.2023.1225891

8、Cui Binjing, Zhu Zhu, Meirong Wang*, Shu Zhou and Shunwu Zhou, 2023. Effects of the trends in spring sensible heating over the Tibetan Plateau during different stages on precipitation in China. Atmosphere, 14, 812.

9、Zhu zhu, Meirong Wang*, Jun Wang, Xulin Ma, Jingjia Luo and Xiuping Yao, 2023. Diurnal variation characteristics of the surface sensible heat flux over the Tibetan Plateau. Atmosphere, 14, 128.

2022

1、Zhou Shu, Sun Fang, Wang Meirong*, Zhou Shunwu*, and Qing Yiyu. 2022. Effects of Atmospheric Heat Source on the Tibetan Plateau Vortex in Different Stages: A Case Study in June 2016. Atmosphere, 2022,13,689. https:// doi.org/10.3390/atmos13050689

2、王美蓉*，周顺武，孙阳，王军，马淑俊，2021.CMIP6全球气候模式对青藏高原中东部地表感热通量模拟能力评估[J].大气科学，46(5).

孙芳，周顺武*，王美蓉，等，2022. 初夏东北移高原低涡活动特征. 气象，48(3): 324–333.

3、Wang, J*., Jiang, F., Ju, W., Wang, M., Sitch, S., Arora, V. K., et al. (2022). Enhanced India-Africa carbon uptake and Asia-Pacific carbon release associated with the 2019 extreme positive Indian Ocean dipole. Geophysical Research Letters, 49, e2022GL100950. https://doi. org/10.1029/2022GL100950

4、Sun Fang, Zhou Shunwu*, Yang Cheng, Ma Xulin, Wang Meirong, Sun Yang, and Zhou Shu. (2022). Activity characteristics of the northeast moving Tibetan Plateau vortices in summer. Atmospheric Research, 272, 106141.

2021

1、Wang, M., Wang, J., Cai, Q., Zeng, N., Lu, X., Yang, R., et al. (2021). Considerable uncertainties in simulating land carbon sinks induced by different precipitation products. Journal of Geophysical Research: Biogeosciences, 126, e2021JG006524. https://doi.org/10.1029/2021JG006524. 1/10

2、Wang M. R.*,William K. M. Lau*, and J. Wang, 2021: Impact of Middle East dust on subseasonal-to-seasonal variability of the Asian summer monsoon, Clim. Dyn., 57: 37–54, DOI: 10.1007/s00382-021-05694-z

3、Wang, J., Wang, M., Kim, J.-S., Joiner, J., Zeng, N., Jiang, F., et al. (2021). Modulation of land photosynthesis by the Indian Ocean Dipole: Satellite- based observations and CMIP6 future projections. Earth's Future, 9, e2020EF001942. https://doi. org/10.1029/2020EF001942.

2020

1、钟珊珊，贾巧，王美蓉，等，2020. 夏季青藏高原大气热源准双周振荡及其传播途径[J].大气科学学报，43( 3) : 495-505.

2、Guo D*, P. J. Shen, C. H. Shi*, Wang M. R.*, Y. Liu, C. X. Zhang, and W. W. Li, 2020: Calculation of the vertical velocity in the Asian summer monsoon anticyclone region using the thermodynamic method with in situ and satellite data, Front. Earth Sci, 8(96), doi: 10.3389/feart. 2020. 00096. 10/10

3、单幸，周顺武，王美蓉，郑丹，王传辉，2020: 在ENSO不同位相下青藏高原春季感热对华南盛夏降水的影响[J].热带气象学报, 36(1):60-71.

2019

1、Wang M. R.*, J. Wang, and D. L. Chen, et al., 2019: Recent recovery of the boreal spring sensible heating over the Tibetan Plateau will continue in CMIP6 future projections, Environ. Res. Lett, 14, 124066.

2、Wang M. R.*, J. Wang*, A. M. Duan, J. Yang, and Y. M. Liu, 2019: Quasi-biweekly impact of the atmospheric heat source over the Tibetan Plateau on summer rainfall in eastern China, Climate Dynamics., 53, 4489-4504.

3、王美蓉*, 郭栋, 钟姗姗. 2019: 多源资料在青藏高原大气热源计算上的适用性分析, 气象, 45(12):1718-1726.

4、单幸, 周顺武*, 王美蓉, 等. 2019: 青藏高原大气热力异常对西风急流的影响, 气象科学, 39(2):206-213.

2018

1、Wang M. R., J. Wang, A. M. Duan, Y. M. Liu, and S. W. Zhou, 2018: Coupling of the Quasi-Biweekly Oscillation of the Tibetan Plateau summer monsoon with the Arctic Oscillation, Geophysical Research Letters, 45, DOI: 10.1029/2018GL077136.

2、王美蓉，周顺武，贾建颖，2018: 《气象统计方法》教学体会，教育教学论坛，10，176-178.

3、Wang J., N. Zeng, and M. R. Wang, et al., 2018: Contrasting interannual atmospheric CO2 variabilities and their terrestrial mechanisms for two types of El Ninos, Atmos. Chem. Phys., 18, 10333-10345.

4、Wang J., N. Zeng, and M. R. Wang, 2018: Contrasting terrestrial carbon cycle responses to the 1997/98 and 2015/16 extreme El Nino events, Earth System Dynamics, 9, 1-14.

2017

Wang M. R., J. Wang, and A. M. Duan, 2017: Propagation and mechanisms of the quasi-biweekly oscillation over the Asian summer monsoon region. J. Meteor. Res., 31(2), 1–16, doi: 10.1007/s13351-017-6131- 5.

2016

Wang J., N. Zeng, and M. R. Wang, 2016: Interannual variability of the atmospheric CO2 growth rate: roles of precipitation and temperature, Biogeosciences, 13, 2339-2352.

刘炜，周顺武，王美蓉，单幸，刘新，1979-2008年青藏高原东南部降水的低频振荡统计特征，干旱气象，2016，34(4)：631-639

2015

Wang M. R., and A. M. Duan, 2015: Quasi-Biweekly Oscillation over the Tibetan Plateau and Its Link with the Asian Summer Monsoon, J. Climate, 28, 4921-4940.

2014

Duan A. M., M. R. Wang, and Z. X. Xiao, 2014: Uncertainties in quantitatively estimating the atmospheric heat source over the Tibetan Plateau, Atmos. Oceanic Sci. Lett., 7(1): 28-33.

段安民，肖志祥，吴国雄，王美蓉，青藏高原冬春积雪影响亚洲夏季风的研究进展，气象与环境科学，2014，37：94-101

2013

Duan A. M., M. R. Wang, Y. H. Lei, and Y. F. Cui, 2013: Trends in summer rainfall over China associated with the Tibetan Plateau sensible heat source during 1980-2008, J. Climate, 26: 261-275.

2012

Wang M. R., S. W. Zhou, and A. M. Duan. 2012: Trend in the atmospheric heat source over the central and eastern Tibetan Plateau during recent decades: Comparison of observations and reanalysis data, Chin. Sci. Bull., 57, 548-557.

周顺武，王传辉，吴萍，王美蓉，青藏高原强降水日数的时空分布特征，干旱区地理，2012，25(1)：23-31

周顺武，杨双艳，张人禾，李慧，王美蓉，近30年青藏高原臭氧总量亏损的可能原因及其与对流层顶高度的联系，高原气象，2012，31(6)：1471-1478

2011

Duan A. M., F. Li, M. R. Wang, and G. X. Wu, 2011: Persistent weakening trend in the spring sensible heat source over the Tibetan Plateau and its impact on the Asian summer monsoon, J. Climate, 24: 5671-5682.