袁東亮，男，博士，博士生導(dǎo)師，享受?chē)?guó)務(wù)院政府特殊津貼專(zhuān)家?，F(xiàn)任自然資源部第一海洋研究所研究員。主要研究領(lǐng)域：海洋環(huán)流與氣候動(dòng)力學(xué)，包括：熱帶太平洋和印度洋海洋環(huán)流和海氣耦合動(dòng)力學(xué)，印尼貫穿流動(dòng)力學(xué)，大洋環(huán)流動(dòng)力學(xué)及其熱鹽輸運(yùn)過(guò)程與通量，邊緣海與陸架環(huán)流動(dòng)力學(xué)及其物質(zhì)輸運(yùn)過(guò)程與通量，非線(xiàn)性動(dòng)力系統(tǒng)研究，大規(guī)模數(shù)值模擬與四維同化，衛(wèi)星海洋學(xué)，等等。發(fā)現(xiàn)了全球大洋中最長(zhǎng)、最強(qiáng)的赤道外次表層潛流，命名之為太平洋北赤道次表層流（NESC）。擔(dān)任過(guò)國(guó)家杰青、國(guó)家重大科學(xué)研究計(jì)劃（973）項(xiàng)目、中科院海洋專(zhuān)項(xiàng)項(xiàng)目A等國(guó)家級(jí)項(xiàng)目負(fù)責(zé)人。曾榮獲山東省國(guó)際合作獎(jiǎng)、山東省留學(xué)人員回國(guó)創(chuàng)業(yè)獎(jiǎng)、山東省自然科學(xué)2等獎(jiǎng)、海洋科學(xué)技術(shù)獎(jiǎng)特等獎(jiǎng)等獎(jiǎng)項(xiàng)。

      1. Jing Wang, Shouwen Zhang*, Hua Jiang, D. Yuan*, 2022: Efects of 2019 subsurface Indian Ocean initialization on the forecast of the 2020/2021 La Ni?a event.Climate Dynamics, https://doi.org/10.1007/s00382-022-06442-7 

      2. Zhang, Z., Wang, J.*, & Yuan, D. * 2022: Mixed layer salinity balance in the eastern tropical Indian Ocean. Journal of Geophysical Research: Oceans, 127, e2021JC018229. https://doi.org/10.1029/2021JC018229  

      3. Yuan D.#* , X. Yin#, X Li#, Corry Corvianawatie, Z Wang,Y Li, Y Yang, et al., 2022: A Maluku Sea intermediate western boundary current connecting Pacific Ocean circulation to the Indonesian Throughflow, Nature Communications, 13:2093, https://doi.org/10.1038/s41467-022-29617-6  

      4. Li X., Yuan D.*, Li Y., Wang Z., Wang J., Hu X., Yang Y., et al. 2021, Moored observations of currents and water mass properties between Talaud and Halmahera Islands at the entrance of the Indonesian seas, J. Phys. Oceanogr., 51(12):3557-3572.

      5. Zhao Xia, Dongliang Yuan*, 2021: Evaluation of intraseasonal wind rectification on recent Indian Ocean dipole events using LICOM, Climate Dynamics, https://link.springer.com/article/10.1007/s00382-021-05943-1.

      6. Hao Jiajia, Yuan Dongliang*, Tian Di, Su Jian, Phlmann Thomas (2021) Long-term changes of cross-shelf transports in the Yellow and East China Seas under different greenhouse gases emission scenarios. Climate Dynamics, https://doi.org/10.1007/s00382-021-06045-8

      7. Li, M., Yuan, D.*, Gordon, A. L., Gruenburg, L., Li, X., Li, R., Yin, X., Yang, Y.*, Corvianatie, C., Wei, J., Yang, S. 2021: A strong sub-thermocline intrusion of the North Equatorial Subsurface Current into the Makassar Strait in 2016-2017. Geophysical Research Letters, 48, e2021GL092505, 10.1029/2021GL092505

      8. Li X., Yuan D.*, Li Y., Wang Z., Wang J., Hu X., Yang Y., et al. 2021, Moored observations of currents and water mass properties between Talaud and Halmahera Islands at the entrance of the Indonesian seas, J. Phys. Oceanogr., 51(12):3557-3572.

      9. Li, X., Y. Yang, R. Li, L. Zhang, and, D. Yuan*, 2020: Structure and dynamics of the Pacific North Equatorial Subsurface Current. Sci. Rep., 10, 11758, 10.1038/s41598-020-68605-y.

      10. Yang, Y., X. Li, J. Wang, and, D. Yuan*, 2020: Seasonal variability and dynamics of the Pacific North Equatorial Subsurface Current. J. Phys. Oceanogr., 50(9), 2457-2474, 10.1175/JPO-D-19-0261.1.

      11. Li, X., D. Yuan*, Z. Wang, et al., 2020: Moored observations of transport and variability of Halmahera Sea currents. J. Phys. Oceanogr., 50(2), 471-488, doi: 10.1175/JPO-D-19-0109.1.

      12. Yuan, D., X. Song, Y. Yang, and W. K. Dewar, 2019: Dynamics of Mesoscale Eddies Interacting With a Western Boundary Current Flowing by a Gap, J. Geophys. Res.: Oceans, 10.1029/2019JC014949.

      13. Yuan D.*, et al., 2018: Observed Transport Variations in the Maluku Channel of the Indonesian Seas Associated with Western Boundary Current Changes, J. Phys. Oceanogr., 48: 1803-1813, DOI: 10.1175/JPO-D-17-0120.1.

      14. Yuan D.*, J. Hao, J. Li, and L. He, 2018: Cross-shelf carbon transport under different greenhouse gas emission scenarios in the East China Sea during winter, Sci. China-Earth Sci., 61(6), 659-667.

      15. Zhou H., D. Yuan*, L. Yang, X. Li, and W. K. Dewar, 2018: Decadal variability of the meridional geostrophic transport in the upper tropical North Pacific Ocean, J. Phys. Oceanogr., 31(15): 5891-5910.

      16. Zhao, X. D. Yuan*, G. Yang, J. Wang, H. Liu, R. Zhang, and W. Han, 2018: Interannual variability and dynamics of intraseasonal wind rectification in the equatorial Pacific Ocean, Clim. Dyn., 52, 4351-4369.

      17. Yuan D.*, X. Hu, P. Xu, X. Zhao, Y. Masumoto, W. Han, 2018: The IOD-ENSO precursory teleconnection over the tropical Indo-Pacific Ocean: dynamics and long-term trends under global warming. J. Oceanol.. Limnol., 36(1), 4-19.

      18. Yuan, D.*, Y. Li, B. Wang, L. He, and N. Hirose, 2017: Coastal circulation in the southwestern Yellow Sea in the summers of 2008 and 2009, Cont. Shelf Res., 143, 101-117.

      19. Wang, J., and D. Yuan*, 2015: Roles of western and eastern boundary reflections in the interannual sea level variations during negative Indian Ocean Dipole events. J. Phys. Oceanogr., 45, 1804-1821, DOI: 10.1175/JPO-D-14-0124.1.

      20. Yuan, D.*, Z. Zhang, P.C. Chu and W. K. Dewar, 2014: Geostrophic Circulation in the Tropical North Pacific Ocean Based on Argo Profiles. J. Phys. Oceanogr., 44, 558-575, doi: 10.1175/JPO-D-12-0230.1.

      21. Wang, Z., D. Yuan*, 2014: Multiple equilibria and hysteresis of two unequal transport western boundary currents colliding at a gap. J. Phys. Oceanogr., 44, 1873-1885, doi: 10.1175/JPO-D-13-0234.1.

      22. Yuan, D.*, H. Zhou, and X. Zhao, 2013: Interannual climate variability over the tropical Pacific Ocean induced by Indian Ocean Dipole through Indonesian Throughflow. J. Climate, 2845-2861, doi: 10.1175/JCLI-D-12-00117.1.

      23. Wang, Z., and D. Yuan*, 2012: Nonlinear Dynamics of Two Western Boundary Currents Colliding at a Gap. J. Phys. Oceanogr., 42(11), 2030-2040.

      24. Yuan, D.*, J. Wang, T. Xu, P. Xu, H. Zhou, X. Zhao, Y. Luan, W. Zheng, Y. Yu, 2011: Forcing of Indian Ocean Dipole on the interannual variations of the tropical Pacific Ocean: Roles of the Indonesian Throughflow. J. Clim., 24, 3593-3608.

      25. Yuan, D.*, and Z. Wang, 2011: Hysteresis and Dynamics of a Western Boundary Current Flowing by a Gap Forced by Impingement of Meso-scale Eddies. J. Phys. Oceanogr., 41, 878-888, doi: 10.1175/2010JPO4489.1

      26. Yuan, D.*, and Y. Hsueh, 2010: Dynamics of the cross-shelf circulation in the Yellow and East China Seas in winter. Deep Sea Research II, 57(19-20), 1745-1761.

  獲獎(jiǎng)與榮譽(yù)

     (1) 2008年獲國(guó)家杰出青年基金；

     (2) 2009年榮獲“新世紀(jì)百千萬(wàn)人才國(guó)家級(jí)人選”；

     (3) 2011年全球變化研究國(guó)家重大科學(xué)研究計(jì)劃項(xiàng)目首席科學(xué)家；

     (4) 2011年在“百人計(jì)劃”終期評(píng)估獲得優(yōu)秀；

     (5) 2012年獲山東省國(guó)際合作獎(jiǎng)、山東省留學(xué)人員回國(guó)創(chuàng)業(yè)獎(jiǎng)；

     (6) 2013年中科院海洋專(zhuān)項(xiàng)項(xiàng)目負(fù)責(zé)人、享受?chē)?guó)務(wù)院政府特殊津貼；

     (7) 2014年獲得基金委“創(chuàng)新研究群體項(xiàng)目”資助，擔(dān)任學(xué)術(shù)帶頭人，2021年結(jié)題評(píng)估獲得優(yōu)秀；

     (8) 2018年獲得“中國(guó)科學(xué)院大學(xué)地球與行星科學(xué)學(xué)院杰出校友”；“太平洋西邊界流與邊緣海交換的動(dòng)力機(jī)制”榮獲山東省自然科學(xué)2等獎(jiǎng)（排名第一）；“熱帶太平洋西邊界流研究集體”獲得中國(guó)科學(xué)院杰出科技成就獎(jiǎng)（排名第三）；

     (9) 2021年獲得海洋科學(xué)技術(shù)獎(jiǎng) 特等獎(jiǎng) (第一完成人）。

    主持項(xiàng)目

      1. 國(guó)家重點(diǎn)研發(fā)計(jì)劃“全球變化背景下西太平洋環(huán)流與ENSO變異及氣候預(yù)測(cè)研究”項(xiàng)目，擔(dān)任項(xiàng)目負(fù)責(zé)人，2021-2025，744萬(wàn)元；

      2. 國(guó)家自然科學(xué)基金委創(chuàng)新研究群體項(xiàng)目，擔(dān)任項(xiàng)目負(fù)責(zé)人，2015-2020，1200萬(wàn)元；

      3. 國(guó)家自然科學(xué)基金委國(guó)際合作重點(diǎn)基金項(xiàng)目，擔(dān)任項(xiàng)目負(fù)責(zé)人，2018-2022，248萬(wàn)元；

      4. 國(guó)家自然科學(xué)基金委重大研究計(jì)劃-重點(diǎn)支持項(xiàng)目，擔(dān)任項(xiàng)目負(fù)責(zé)人，2019-2022, 253萬(wàn)元；

      5. 中國(guó)科學(xué)院戰(zhàn)略性先導(dǎo)科技專(zhuān)項(xiàng)B，擔(dān)任項(xiàng)目負(fù)責(zé)人，2020-2024，625萬(wàn)元；

      6. 曾經(jīng)擔(dān)任：國(guó)家杰青、國(guó)家重大科學(xué)研究計(jì)劃（973）項(xiàng)目、中科院海洋專(zhuān)項(xiàng)項(xiàng)目A等國(guó)家級(jí)項(xiàng)目負(fù)責(zé)人。

     科技貢獻(xiàn)

      1. 發(fā)現(xiàn)了全球大洋中最長(zhǎng)、最強(qiáng)的赤道外次表層潛流，命名之為太平洋北赤道次表層流（NESC），位于太平洋北赤道逆流之下，向西流動(dòng)，并進(jìn)入印尼貫穿流，是中、東赤道太平洋水團(tuán)進(jìn)入印尼海以及印度洋的唯一通道，是熱帶海洋環(huán)流和全球海洋大輸送帶的重要補(bǔ)充。NESC的發(fā)現(xiàn)，表明南北太平洋中層水團(tuán)經(jīng)過(guò)印尼貫穿流進(jìn)入印度洋，并完成上浮至海平面的過(guò)程，該路徑是對(duì)全球通風(fēng)熱鹽環(huán)流的重要新認(rèn)識(shí)。

      2. 發(fā)現(xiàn)來(lái)自南太平洋的印尼貫穿流分支，經(jīng)哈馬黑拉海進(jìn)入印尼海，表明南太平洋翻轉(zhuǎn)環(huán)流加入全球海洋大輸送帶，改變了傳統(tǒng)認(rèn)識(shí)格局。還發(fā)現(xiàn)印尼馬魯古海上層向北的平均輸運(yùn)，以及薩武海峽的次溫躍層潛流，為印尼貫穿流逆流的存在提供了關(guān)鍵證據(jù)。

      3. 提出了熱帶印度洋偶極子通過(guò)印尼貫穿流影響太平洋暖池?zé)崃Τ浞藕虴NSO演變的“海洋通道”機(jī)制，顯著提升了ENSO預(yù)報(bào)技能。

      4. 發(fā)現(xiàn)了羅斯貝波在西邊界的強(qiáng)非線(xiàn)性反射過(guò)程，揭示其與跨隙流動(dòng)的西邊界流遲滯和分岔過(guò)程的非線(xiàn)性相互作用機(jī)制，并使用衛(wèi)星遙感和現(xiàn)場(chǎng)潛標(biāo)數(shù)據(jù)提供確鑿觀測(cè)證據(jù)，揭示了西邊界反射在ENSO和印度洋偶極子演變中的滯后負(fù)反饋機(jī)；發(fā)現(xiàn)了全球熱帶大洋的非Sverdrup環(huán)流結(jié)構(gòu)，指出其可能是由環(huán)流非線(xiàn)性過(guò)程驅(qū)動(dòng)的。

      5. 發(fā)現(xiàn)了我國(guó)閩浙沿岸的跨陸架穿刺鋒面現(xiàn)象、南海深層“三明治”環(huán)流結(jié)構(gòu)、呂宋海峽黑潮的季節(jié)內(nèi)變異特征和非線(xiàn)性遲滯動(dòng)力機(jī)制等邊緣?，F(xiàn)象和過(guò)程，揭示了黑潮與中國(guó)近海水交換的三個(gè)主要通道：跨陸架環(huán)流、穿刺鋒面和呂宋海峽交換。