Abstract
The linkage between the sea ice concentration (SIC) over the Barents-Kara Seas in November–December (SIC_BKS_ND) and the stratospheric polar vortex (SPV) in subsequent January (SPV_Jan) is investigated. It is found that SIC_BKS_ND is positively (negatively) correlated with SPV_Jan for the period 1979–1995 (1996–2009). Further analyses reveal that, during 1979–1995 (1996–2009), SIC_BKS_ND is relatively higher (lower), accompanied by smaller (larger) interannual variability with its center shifting northwest (southeast). Meanwhile, the polar front jet waveguide is relatively stronger (weaker). The simultaneous anomalous eastward-propagating Rossby waves excited by anomalously low SIC_BKS_ND are stronger (weaker), which results in the stronger (weaker) negative-positive-negative wave-train structure of geopotential height anomalies over Eurasia, with the location of these anomalous height centers shifting remarkably westward (eastward). Such changes tend to enhance (suppress) vertically propagating tropospheric planetary waves into the lower stratosphere at high-latitude via constructive (destructive) interference of anomalous tropospheric wave-train structure with the climatological planetary waves, subsequently weakening (strengthening) SPV_Jan. However, in conjunction with anomalously high SIC_BKS_ND, the interference of the tropospheric wave-train structure anomalies and their climatologies shows an opposite distribution to that of low SIC_BKS_ND anomalies, which leads to a strong (weak) SPV_Jan anomaly during 1979–1995 (1996–2009).
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Andrews, D. G., J. R. Holton, and C. B. Leovy, 1987: Middle Atmosphere Dynamics. Academic Press, Orlando, 489 pp.
Baldwin, M. P., and T. J. Dunkerton, 2001: Stratospheric harbingers of anomalous weather regimes. Science, 294, 581–584, doi: https://doi.org/10.1126/science.1063315.
Chen, X. D., and D. H. Luo, 2017: Arctic sea ice decline and continental cold anomalies: Upstream and downstream effects of Greenland blocking. Geophys. Res. Lett., 44, 3411–3419, doi: https://doi.org/10.1002/2016GL072387.
Cohen, J., J. Jones, J. C. Furtado, et al., 2013: Warm Arctic, cold continents: A common pattern related to Arctic sea ice melt, snow advance, and extreme winter weather. Oceanography, 26, 152–160, doi: https://doi.org/10.5670/oceanog.2013.70.
Cohen, J., J. A. Screen, J. C. Furtado, et al., 2014: Recent Arctic amplification and extreme mid-latitude weather. Nat. Geosci., 7, 627–637, doi: https://doi.org/10.1038/ngeo2234.
Cohen, J., X. Zhang, J. Francis, et al., 2020: Divergent consensuses on Arctic amplification influence on midlatitude severe winter weather. Nat. Climate Change, 10, 20–29, doi: https://doi.org/10.1038/s41558-019-0662-y.
Comiso, J. C., C. L. Parkinson, R. Gersten, et al., 2008: Accelerated decline in the Arctic sea ice cover. Geophys. Res. Lett., 35, L01703, doi: https://doi.org/10.1029/2007GL031972.
Dai, H. X., K. Fan, and J. P. Liu, 2019: Month-to-month variability of winter temperature over northeast China linked to sea ice over the Davis Strait-Baffin bay and the Barents-Kara sea. J. Climate, 32, 6365–6384, doi: https://doi.org/10.1175/JCLI-D-18-0804.1.
Ding, S. Y., and B. Y. Wu, 2021: Linkage between autumn sea ice loss and ensuing spring Eurasian temperature. Climate Dyn., 57, 2793–2810, doi: https://doi.org/10.1007/s00382-021-05839-0.
Edmon, H. J. Jr., B. J. Hoskins, and M. E. Mcintyre, 1980: Eliassen- palm cross sections for the troposphere. J. Atmos. Sci., 37, 2600–2616, doi: https://doi.org/10.1175/1520-0469(1980)037<2600:epcsft>2.0.co;2.
Eyring, V., S. Bony, G. A. Meehl, et al., 2016: Overview of the coupled model intercomparison project phase 6 (CMIP6) experimental design and organization. Geosci. Model Dev., 9, 1937–1958, doi: https://doi.org/10.5194/gmd-9-1937-2016.
Fan, K., Z. M. Xie, H. J. Wang, et al., 2018: Frequency of spring dust weather in North China linked to sea ice variability in the Barents Sea. Climate Dyn., 51, 4439–4450, doi: https://doi.org/10.1007/s00382-016-3515-7.
Fletcher, C. G., and P. J. Kushner, 2011: The role of linear interference in the annular mode response to tropical SST forcing. J. Climate, 24, 778–794, doi: https://doi.org/10.1175/2010JCLI3735.1.
Gao, Y. Q., J. Q. Sun, F. Li, et al., 2015: Arctic sea ice and Eurasian climate: A review. Adv. Atmos. Sci., 32, 92–114, doi: https://doi.org/10.1007/s00376-014-0009-6.
Garfinkel, C. I., D. L. Hartmann, and F. Sassi, 2010: Tropospheric precursors of anomalous Northern Hemisphere stratospheric polar vortices. J. Climate, 23, 3282–3299, doi: https://doi.org/10.1175/2010JCLI3010.1.
Guo, D., Y. Q. Gao, I. Bethke, et al., 2014: Mechanism on how the spring Arctic sea ice impacts the East Asian summer monsoon. Theor. Appl. Climatol., 115, 107–119, doi: https://doi.org/10.1007/s00704-013-08726.
Han, T. T., M. H. Zhang, J. W. Zhu, et al., 2021: Impact of early spring sea ice in Barents Sea on midsummer rainfall distribution at Northeast China. Climate Dyn., 57, 1023–1037, doi: https://doi.org/10.1007/s00382-021-05754-4.
Hartmann, D. L., J. M. Wallace, V. Limpasuvan, et al., 2000: Can ozone depletion and global warming interact to produce rapid climate change. Proc. Natl. Acad. Sci. USA, 97, 1412–1417, doi: https://doi.org/10.1073/pnas.97.4.1412.
He, S. P., Y. Q. Gao, T. Furevik, et al., 2018: Teleconnection between sea ice in the Barents Sea in June and the Silk Road, Pacific-Japan and East Asian rainfall patterns in August. Adv. Atmos. Sci., 35, 52–64, doi: https://doi.org/10.1007/s00376-017-7029-y.
Hu, D. Z., Y. P. Guo, and Z. Y. Guan, 2019: Recent weakening in the stratospheric planetary wave intensity in early winter. Geophys. Res. Lett., 46, 3953–3962, doi: https://doi.org/10.1029/2019GL082113.
Jaiser, R., K. Dethloff, and D. Handorf, 2013: Stratospheric response to Arctic sea ice retreat and associated planetary wave propagation changes. Tellus A: Dynamic Meteorology and Oceanography, 65, 19375, doi: https://doi.org/10.3402/tellusa.v65i0.19375.
Ji, L. Q., and K. Fan, 2019: Climate prediction of dust weather frequency over northern China based on sea-ice cover and vegetation variability. Climate Dyn., 53, 687–705, doi: https://doi.org/10.1007/s00382-018-04608-w.
Kalnay, E., M. Kanamitsu, and R. Kistler, et al., 1996: The NCEP/NCAR 40-year reanalysis project. Bull. Amer. Meteor. Soc., 77, 437–472, doi: https://doi.org/10.1175/1520-0477(1996)077<0437:tnyrp>2.0.co;2.
Kim, B. M., S. W. Son, S. K. Min, et al., 2014: Weakening of the stratospheric polar vortex by Arctic sea-ice loss. Nat. Commun., 5, 4646, doi: https://doi.org/10.1038/ncomms5646.
Kobayashi, S., Y. Ota, Y. Harada, et al., 2015: The JRA-55 reanalysis: General specifications and basic characteristics. J. Meteor. Soc. Japan, 93, 5–48, doi: https://doi.org/10.2151/jmsj.2015-001.
Koenigk, T., M. Caian, G. Nikulin, et al., 2016: Regional Arctic sea ice variations as predictor for winter climate conditions. Climate Dyn., 46, 317–337, doi: https://doi.org/10.1007/s00382-015-2586-1.
Li, H. X., H. P. Chen, H. J. Wang, et al., 2018: Can Barents sea ice decline in spring enhance summer hot drought events over northeastern China. J. Climate, 31, 4705–4725, doi: https://doi.org/10.1175/JCLI-D-17-0429.1.
Li, Y. Y., and Z. C. Yin, 2020: Melting of perennial sea ice in the Beaufort sea enhanced its impacts on early-winter haze pollution in North China after the mid-1990s. J. Climate, 33, 5061–5080, doi: https://doi.org/10.1175/JCLI-D-19-0694.1.
McKenna, C. M., T. J. Bracegirdle, E. F. Shuckburgh, et al., 2018: Arctic sea ice loss in different regions leads to contrasting northern hemisphere impacts. Geophys. Res. Lett., 45, 945–954, doi: https://doi.org/10.1002/2017GL076433.
Mori, M., M. Watanabe, H. Shiogama, et al., 2014: Robust Arctic sea-ice influence on the frequent Eurasian cold winters in past decades. Nat. Geosci., 7, 869–873, doi: https://doi.org/10.1038/ngeo2277.
Nakamura, T., K. Yamazaki, K. Iwamoto, et al., 2015: A negative phase shift of the winter AO/NAO due to the recent Arctic sea-ice reduction in late autumn. J. Geophys. Res.: Atmos., 120, 3209–3227, doi: https://doi.org/10.1002/2014JD022848.
Nakamura, T., K. Yamazaki, K. Iwamoto, et al., 2016: The stratospheric pathway for Arctic impacts on midlatitude climate. Geophys. Res. Lett., 43, 3494–3501, doi: https://doi.org/10.1002/2016GL068330.
Nishii, K., H. Nakamura, and Y. J. Orsolini, 2010: Cooling of the wintertime Arctic stratosphere induced by the western Pacific teleconnection pattern. Geophys. Res. Lett., 37, L13805, doi: https://doi.org/10.1029/2010GL043551.
Polvani, L. M., and D. W. Waugh, 2004: Upward wave activity flux as a precursor to extreme stratospheric events and subsequent anomalous surface weather regimes. J. Climate, 17, 3548–3554, doi: https://doi.org/10.1175/1520-0442(2004)017<3548:UWAFAA>2.0.CO;2.
Randel, W. J., 1987: A study of planetary waves in the southern winter troposphere and stratosphere. Part I: Wave structure and vertical propagation. J. Atmos. Sci., 44, 917–935, doi: https://doi.org/10.1175/1520-0469(1987)044<0917:asopwi>2.0.co;2.
Rayner, N. A., D. E. Parker, E. B. Horton, et al., 2003: Global analyses of sea surface temperature, sea ice, and night marine air temperature since the late nineteenth century. J. Geophys. Res.: Atmos., 108, 4407, doi: https://doi.org/10.1029/2002JD002670.
Screen, J. A., and I. Simmonds, 2010: The central role of diminishing sea ice in recent Arctic temperature amplification. Nature, 464, 1334–1337, doi: https://doi.org/10.1038/nature09051.
Smith, K. L., C. G. Fletcher, and P. J. Kushner, 2010: The role of linear interference in the annular mode response to extratropical surface forcing. J. Climate, 23, 6036–6050, doi: https://doi.org/10.1175/2010JCLI3606.1.
Sun, L. T., C. Deser, and R. A. Tomas, 2015: Mechanisms of stratospheric and tropospheric circulation response to projected Arctic Sea ice loss. J. Climate, 28, 7824–7845, doi: https://doi.org/10.1175/JCLI-D15-0169.1.
Takaya, K., and H. Nakamura, 2001: A formulation of a phase-independent wave-activity flux for stationary and migratory quasigeostrophic eddies on a zonally varying basic flow. J. Atmos. Sci., 58, 608–627, doi: https://doi.org/10.1175/1520-0469(2001)058<0608:AFOAPI>2.0.CO;2.
Tang, Q. H., X. J. Zhang, X. H. Yang, et al., 2013: Cold winter extremes in northern continents linked to Arctic sea ice loss. Environ. Res. Lett., 8, 014036, doi: https://doi.org/10.1088/17489326/8/1/014036.
Vihma, T., 2014: Effects of Arctic sea ice decline on weather and climate: a review. Surv. Geophy., 35, 1175–1214, doi: https://doi.org/10.1007/s10712-014-9284-0.
Wang, H. J., H. P. Chen, and J. P. Liu, 2015: Arctic sea ice decline intensified haze pollution in eastern China. Atmos. Oceanic Sci. Lett., 8, 1–9, doi: https://doi.org/10.3878/AOSL20140081.
Wang, L., R. H. Huang, L. Gu, et al., 2009: Interdecadal variations of the east Asian winter monsoon and their association with quasi-stationary planetary wave activity. J. Climate, 22, 4860–4872, doi: https://doi.org/10.1175/2009JCLI2973.1.
Woo, S.-H., B.-M. Kim and J.-S. Kug, 2015: Temperature variation over East Asia during the lifecycle of weak stratospheric polar vortex. J. Climate, 28, 5857–5872, doi: https://doi.org/10.1175/JCLID-14-00790.1.
Wu, B. Y., J. Z. Su, and R. H. Zhang, 2011: Effects of autumn- winter Arctic sea ice on winter Siberian High. Chinese Sci. Bull., 56, 3220–3228, doi: https://doi.org/10.1007/s11434-011-4696-4.
Wu, Y. T., and K. L. Smith, 2016: Response of northern hemisphere midlatitude circulation to Arctic amplification in a simple atmospheric general circulation model. J. Climate, 29, 2041–2058, doi: https://doi.org/10.1175/JCLI-D-15-0602.1.
Xu, M., W. S. Tian, J. K. Zhang, et al., 2021: Impact of sea ice reduction in the Barents and Kara Seas on the variation of the East Asian trough in late winter. J. Climate, 34, 1081–1097, doi: https://doi.org/10.1175/JCLI-D-20-0205.1.
Yang, X.-Y., X. J. Yuan, and M. F. Ting, 2016: Dynamical link between the Barents-Kara sea ice and the Arctic Oscillation. J. Climate, 29, 5103–5122, doi: https://doi.org/10.1175/JCLI-D-15-0669.1.
Zhang, J. K., W. S. Tian, M. P. Chipperfield, et al., 2016: Persistent shift of the Arctic polar vortex towards the Eurasian continent in recent decades. Nat. Climate Change, 6, 1094–1099, doi: https://doi.org/10.1038/nclimate3136.
Zhang, P. F., Y. T. Wu, and K. L. Smith, 2018a: Prolonged effect of the stratospheric pathway in linking Barents-Kara Sea sea ice variability to the midlatitude circulation in a simplified model. Climate Dyn., 50, 527–539, doi: https://doi.org/10.1007/s00382-017-3624-y.
Zhang, P. F., Y. T. Wu, I. R. Simpson, et al., 2018b: A stratospheric pathway linking a colder Siberia to Barents-Kara Sea sea ice loss. Sci. Adv., 4, eaat6025, doi: https://doi.org/10.1126/sciadv.aat6025.
Zhang, P. F, Y. T. Wu, G. Chen, et al., 2020: North American cold events following sudden stratospheric warming in the presence of low Barents-Kara Sea sea ice. Environ. Res. Lett., 15, 124017, doi: https://doi.org/10.1088/1748-9326/abc215.
Zhang, R. N., and J. A. Screen, 2021: Diverse Eurasian winter temperature responses to Barents-Kara sea ice anomalies of different magnitudes and seasonality. Geophys. Res. Lett., 48, e2021GL092726, doi: https://doi.org/10.1029/2021GL092726.
Zhang, R. N., C. H. Sun, R. H. Zhang, et al., 2019: Role of Eurasian snow cover in linking winter-spring Eurasian coldness to the autumn Arctic sea ice retreat. J. Geophys. Res. Atmos., 124, 9205–9221, doi: https://doi.org/10.1029/2019JD030339.
Zwally, H. J., and P. Gloersen, 2008: Arctic sea ice surviving the summer melt: Interannual variability and decreasing trend. J. Glaciol., 54, 279–296, doi: https://doi.org/10.3189/002214308784886108.
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Supported by the National Natural Science Foundation of China (41730964 and 42088101) and Innovation Group Project of Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai) (311021001).
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Zhou, H., Fan, K. Decadal Change of the Linkage between Sea Ice over the Barents-Kara Seas in November-December and the Stratospheric Polar Vortex in Subsequent January. J Meteorol Res 36, 601–617 (2022). https://doi.org/10.1007/s13351-022-1225-0
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DOI: https://doi.org/10.1007/s13351-022-1225-0