Northern Hemisphere sea ice variability: lag structure and its implications

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Ukita, Jinro ; Honda, Meiji ; Nakamura, Hisashi ; Tachibana, Yoshihiro ; Cavalieri, Donald J. ; Parkinson, Claire L. ; Koide, Hiroshi ; Yamamoto, Kentaro (2007)

An analysis of satellite sea-ice records for recent decades reveals a highly coherent spatial and temporal structure of the Northern Hemisphere (NH) wintertime sea-ice variability and its close link to anomalous atmospheric circulation. The dominant mode of the wintertime sea-ice variability is characterized by a double-dipole composed of one dipole over the North Atlantic and the other over the North Pacific, which are mutually correlated interannually. This dominant sea-ice mode is lag correlated with the winter-averaged North Atlantic Oscillation (NAO) index at lags up to two winters when the NAO leads. In the sub-Arctic, significant lead–lag relationships exist between sea-ice extent (SIE) anomalies on regional scales, which are closely associated with atmospheric circulation anomalies. An eastward evolving pattern is identified in regional SIE anomalies from the Labrador to Nordic and farther to the Okhotsk Sea at multi-year time-scales, led by anomalously weak Aleutian and strong Icelandic lows. The results suggest the presence of climate memories over the North Atlantic and Eurasia, which are crucial for recent downward trends in the NH SIE by transforming atmospheric influences into slower changes in sea-ice conditions. The summer Okhotsk high, which leads to a sea-ice reduction along the east Siberian coast and further affects sea-ice conditions over the Arctic Ocean, is a key link between summer Arctic and winter sub-Arctic sea-ice trends. We also conjecture that variations and changes in the NH sea-ice conditions are linked to climate variability in the tropics.
  • References (57)
    57 references, page 1 of 6

    Aagaard, K. and Carmack, E. C. 1989. The role of sea ice and other fresh waters in the Arctic circulation. J. Geophys. Res. 94, 14485-14498.

    Bengtsson, L., Semenov, V. A. and Johannessen, O. M. 2004. The early twentieth-century warming in the Arctic - A possible mechanism. J. Climate 17, 4045-4057.

    Blindheim, J., Borovkov, V., Hansen, B., Malmberg, S.-Aa., Turrell, W. R. and co-authors. 2000. Upper layer cooling and freshening in the Norwegian Sea in relation to atmospheric forcing. Deep-Sea Res. 47, 655-680.

    Bojariu, R. and Gimeno, L. 2003. The role of snow cover fluctuations in multiannual NAO persistence. Geophys. Res. Lett. 30, 1156, doi:10.1029/2002GL01651.

    Cassou, C. and Terry, L. 2001. Dual influence of Atlantic and Pacific SST anomalies on the North Atlantic/Europe winter climate. Geophys. Res. Lett. 28, 3195-3198.

    Cavalieri, D. J., Gloersen, P., Parkinson, C. L., Comiso, J. C. and Zwally, H. J. 1997. Observed hemispheric asymmetry in global sea ice changes. Science 278, 1104-1106.

    Cavalieri, D. J., Parkinson, C. L., Gloersen, P., Comiso, J. C. and Zwally, H. J. 1999. Deriving long-term time series of sea ice Cover from satellite passive-microwave multisensor data sets. J. Geophys. Res. 104, 15803-15814.

    Cavalieri, D. J., Parkinson, C. L. and Vinnikov, K. Y. 2003. 30-year satellite record reveals contrasting Arctic and Antarctic decadal sea ice variability. Geophys. Res. Lett. 30, 1970, doi:10:1029/2003GL018031.

    Chapman, W. L. and Walsh, J. E. 1993. Recent variations of sea ice and air temperature in high latitudes. Bull. Am. Meteorol. Soc. 74, 33- 47.

    Cohen, J. and Entekhabi, D. 1999. Eurasian snow cover variability and Northern Hemisphere climate predictability. Geophys. Res. Lett. 26, 345-348.

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