CHEN Xingrong, LIU Shan, CAI Yi, ZHANG Shouwen. Potential effects of subduction rate in the key ocean on global warming hiatus[J]. Acta Oceanologica Sinica, 2018, 37(3): 63-68. doi: 10.1007/s13131-017-1130-z
Citation: CHEN Xingrong, LIU Shan, CAI Yi, ZHANG Shouwen. Potential effects of subduction rate in the key ocean on global warming hiatus[J]. Acta Oceanologica Sinica, 2018, 37(3): 63-68. doi: 10.1007/s13131-017-1130-z

Potential effects of subduction rate in the key ocean on global warming hiatus

doi: 10.1007/s13131-017-1130-z
  • Received Date: 2017-07-10
  • In this study, the possible effects of subduction rate on global warming hiatus were investigated using Simple Ocean Data Assimilation (SODA) data. This study first analyzed the characteristics of the temporal and spatial distribution of global subduction rate, which revealed that the North Atlantic meridional overturning circulation region and the Antarctic Circumpolar Current region are the two main sea areas with great subduction variations. On this basis, four key areas were selected to explore the relationship between the local subduction rate and the global mean sea surface temperature. In addition, the reason for the variations in subduction rate was preliminarily explored. The results show good correspondence of the subduction of the key areas in the North Atlantic meridional overturning the circulation region and the Antarctic Circumpolar Current region to the global warming hiatus, with the former leading by about 10 years. The subduction process may be a physical mechanism by which the North Atlantic overturning circulation and the Antarctic Circumpolar Current act on the stagnation of global warming. Advection effect plays an important role in the variations in subduction in the key regions. In the Antarctic Circumpolar Current region, the magnitude of sea surface wind stress is closely related to the local changes in subduction.
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  • Balmaseda M A, Trenberth K E, Källén E. 2013. Distinctive climate signals in reanalysis of global ocean heat content. Geophys Res Lett, 40(9): 1754-1759,, doi: 10.1002/grl.50382
    Carton J A, Giese B S. 2008. A reanalysis of ocean climate using simple ocean data assimilation (SODA). Mon Wea Rev, 136(8): 2999-3017
    Chen Xingrong, Cai Yi, Tan Jing, et al. 2014. Research progress on hiatus in the process of global warming. Advances in Earth Science (in Chinese), 29(8): 947-955, doi: 10.11867/j.issn.1001- 8166.2014.08.0947
    Chen Ju, Qu Tangdong, Sasaki Y N, et al. 2010. Anti-correlated variability in subduction rate of the western and eastern north pacific oceans identified by an eddy-resolving ocean GCM. Geophys Res Lett, 37(23): L23608
    Chen Xianyao, Tung K K. 2014. Varying planetary heat sink led to global-warming slowdown and acceleration. Science, 345(6199): 897-903
    Easterling D R, Wehner M F. 2009. Is the climate warming or cooling?.. Geophys Res Lett, 36(8): L08706, doi: 10.1029/2009GL037810
    Foster G, Rahmstorf S. 2011. Global temperature evolution 1979-2010. Environmental Research Letters, 6(4): 044022, doi: 10.1088/1748-9326/6/4/044022
    Guemas V, Doblas-Reyes F J, Andreu-Burillo I, et al. 2013. Retrospective prediction of the global warming slowdown in the past decade. Nature Climate Change, 3(7): 649-653,, doi: 10.1038/nclimate1863
    Heffernan O. 2014. Pacific puzzle. Nature Climate Change, 4(3): 167-169,, doi: 10.1038/nclimate2149
    Huang Ruixin, Qiu Bo. 1994. Three-dimensional structure of the wind-driven circulation in the subtropical North Pacific. J Phys Oceanogr, 24(7): 1608-1622
    Huber M, Knutti R. 2014. Natural variability, radiative forcing and climate response in the recent hiatus reconciled. Nature Geoscience, 7(9): 651-656,, doi: 10.1038/ngeo2228
    Kerr R A. 2009. What happened to global warming? Scientists say just wait a bit. Science, 326(5949): 28-29
    Knight J, Kennedy J J, Folland C, et al. 2009. Do global temperature trends over the last decade falsify climate predictions? [In “state of the climate in 2008”]. Bulletin of the American Meteorological Society, 90(8): S22-S23
    Kosaka Y, Xie Shangping. 2013. Recent global-warming hiatus tied to equatorial Pacific surface cooling. Nature, 501(7467): 403-407,, doi: 10.1038/nature12534
    Liu Chengyan. 2012. Long-term changes of subduction and obduction over the global ocean and their mechanisms in the 20th century (in Chinese) [dissertation]. Qingdao: Ocean University of China
    Liu Qinyu, Hu Haibo, Liu Hailong, et al. 2006. The role of sea surface wind in “subduction” rate variation in north pacific. Oceanologia et Limnologia Sinica (in Chinese), 37(2): 184-192
    Liu Lingling, Huang Ruixin. 2010. The global subduction/obduction rates: their interannual and decadal variability. Journal of Climate, 25(4): 1096-1115
    Liu Chengyan, Wang Zhaomin. 2014. On the response of the global subduction rate to globalwarming in coupled climate models. Advances in Atmospheric Sciences, 31(1): 211-218
    Met Office. 2013a. The Recent Pause in Global Warming (1): What Do Observations of the Climate System Tell Us?. Exeter Devon: Met Office, 1-27
    Met Office. 2013b. The Recent Pause in Global Warming (2): What are the Potential Causes?. Exeter Devon: Met Office, 1-22
    Meehl G A, Arblaster J M, Fasullo J T, et al. 2011. Model-based evidence of deep-ocean heat uptake during surface-temperature hiatus periods. Nature Climate Change, 1(7): 360-364,, doi: 10.1038/nclimate1229
    Meehl G A, Hu Aixue, Arblaster J M, et al. 2013. Externally forced and internally generated decadal climate variability associated with the interdecadal pacific oscillation. Journal of Climate, 26(18): 7298-7310
    Qu Tangdong, Xie Shangping, Mitsudera H, et al. 2002. Subduction of the north pacific mode waters in a global high-resolution GCM. J Phys Oceanogr, 32(3): 746-763
    Qu Tangdong, Zhang Linlin, Schneider N. 2016. North Atlantic subtropical underwater and its year-to-year variability in annual subduction rate during the Argo period. J Phys Oceanogr, 46(6): 1901-1916
    Suga T, Hanawa K, Toba Y. 1989. Subtropical mode water in the 137°E section. J Phys Oceanogr, 19(10): 1605-1619
    Trenberth K E. 2009. An imperative for climate change planning: tracking Earth's global energy. Current Opinion in Environmental Sustainability, 1(1): 19-27
    Trenberth K E, Fasullo J T. 2013. An apparent hiatus in global warming?.. Earth's Future, 1(1): 19-32,, doi: 10.1002/2013ef000165
    Trenberth K E, Fasullo J T, Kiehl J. 2009. Earth's global energy budget. Bulletin of the American Meteorological Society, 90(3): 311-323
    Wang Shaowu, Luo Yong, Zhao Zongci, et al. 2014. How long will the pause of global warming stay again?.. Progressus Inquisitiones de Mutatione Climatis (in Chinese), 10(6): 465-468
    Wang Xiaoyu, Zhao Jinping, Li Tao, et al. 2015. Deep waters warming in the Nordic seas from 1972 to 2013. Acta Oceanologica Sinica, 34(3): 18-24
    Yang Hui, Gong Yuanfa, Yang Guiying. 2017. Correlation between meridional migration of the East Asian jet stream and tropical convection over Indonesia in winter. Satellite Oceanography and Meteorology, 2(1): 60-74
    Yu Kai, Qu Tangdong, Dong Changming, et al. 2015. Effect of subtropical mode water on the decadal variability of the subsurface transport through the Luzon strait in the western Pacific Ocean. Journal of Geophysical Research: Oceans, 120(10): 6829-6842
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