Potential impacts of enhanced tropical cyclone activity on the El Ni?o–Southern Oscillation and East Asian monsoon in the mid-Piacenzian warm period
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  • 英文篇名:Potential impacts of enhanced tropical cyclone activity on the El Ni?o–Southern Oscillation and East Asian monsoon in the mid-Piacenzian warm period
  • 作者:YAN ; Qing ; ZHANG ; Zhongshi ; ZHANG ; Ran
  • 英文作者:YAN Qing;ZHANG Zhongshi;ZHANG Ran;Nansen-Zhu International Research Centre, Institute of Atmospheric Physics, Chinese Academy of Sciences;Department of Atmospheric Science, School of Environmental Studies, China University of Geosciences;Bjerknes Center for Climate Research,Uni Research Climate;Climate Change Research Center, Chinese Academy of Sciences;
  • 关键词:皮亚琴察中期 ; 气候模拟 ; 热带气旋 ; 厄尔尼诺南方涛动
  • 英文关键词:Mid-Piacenzian;;climate modeling;;tropical cyclone;;ENSO
  • 中文刊名:AOSL
  • 英文刊名:大气和海洋科学快报(英文版)
  • 机构:Nansen-Zhu International Research Centre, Institute of Atmospheric Physics, Chinese Academy of Sciences;Department of Atmospheric Science, School of Environmental Studies, China University of Geosciences;Bjerknes Center for Climate Research,Uni Research Climate;Climate Change Research Center, Chinese Academy of Sciences;
  • 出版日期:2019-01-16
  • 出版单位:Atmospheric and Oceanic Science Letters
  • 年:2019
  • 期:v.12
  • 基金:funded by the National Natural Science Foundation of China [grant number 41772179];; the Young Elite Scientists Sponsorship Program by China Association for Science and Technology [grant number 2017QNRC001]
  • 语种:英文;
  • 页:AOSL201901001
  • 页数:11
  • CN:01
  • ISSN:11-5693/P
  • 分类号:3-13
摘要
热带气旋不仅是一种严重的灾害性天气事件,其在气候时间尺度也可通过加强海洋上层垂直混合进而调节全球海洋经向热量输送。基于一个海气耦合模式,本文探讨了强热带气旋活动对皮亚琴察暖期(又称晚上新世暖期;约300万年前)ENSO和东亚季风环流的可能影响。模拟结果表明,热带气旋引起的海洋垂直混合加强可造成热带东太平洋显著增温、温跃层加深,但ENSO年际变率减弱。对东亚季风而言,夏季副热带高压南移且西伸,副热带急流减弱并南移,我国南方西南风加强;冬季东亚大槽加深,副热带急流南移,我国北方偏北风加强。上述模拟结果可增进我们对热带气旋气候反馈作用以及晚上新世暖期全球气候特征的认识。
        Tropical cyclones(TCs) not only passively respond to climate change, but also play an important role in vertical mixing of the upper ocean and in driving oceanic heat transport. Using a fully coupled climate model, the authors investigate the potential e?ect of TC-induced vertical mixing on the El Ni?o–Southern Oscillation(ENSO) and East Asian monsoon in the mid-Piacenzian,during which global TCs are estimated to have been stronger. Sensitivity experiments indicate that the TC-induced oceanic mixing over global storm basins leads to additional warming over the eastern tropical Paci?c and a deeper thermocline in the mid-Piacenzian, whereas it dampens the interannual variability of ENSO. Regarding the East Asian monsoon circulations, low-level(850 hPa) summer and winter winds are intensi?ed in response to enhanced vertical mixing, with a southward/westward shift of the western North Paci?c high and westerly jet in summer and a deepened East Asian trough in winter. These climatic features are largely reproduced in the experiment with enhanced vertical mixing only over the central-eastern North Paci?c. These results may shed light on TC feedbacks associated with vertical mixing and advance our understanding on mid-Piacenzian climate.
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