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1 Wang, M., and J.E. Overland (2009): A sea ice free summer Arctic within 30 years? Geophys. Res. Lett., 36, L07502, doi: 10.1029/2009GL037820.

2 Overland, J.E., and M. Wang (2010): Large-scale atmospheric circulation changes associated with the recent loss of Arctic sea ice. Tellus, 62A, 1–9.

3Honda, M., J. Inoue, and S. Yamane (2009): Influence of low Arctic sea-ice minima on anomalously cold Eurasian winters. Geophys. Res. Lett., 36, L08707, doi:10.1029/2008GL037079.

4Strey, S.T., W. Chapman, and J. Walsh (2009): Effects Of An Extreme Arctic Sea Ice Minimum On the Northern Hemisphere Atmosphere During Late Autumn and Early Winter:, Eos Trans. Eos Trans. AGU, 90(52), Fall Meet. Suppl., Abstract C41A-0421.

5 Schweiger, A.J., R.W. Lindsay, S. Vavrus, and J.A. Francis (2008): Relationships between Arctic sea ice and clouds during autumn. J. Climate, 21, 4799–4810.

6 Serreze, M.C., A.P. Barrett, J.C. Stroeve, D.N. Kindig, and M.M. Holland (2009): The emergence of surface-based Arctic amplification. The Cryosphere, 3, 11–19.

7 Holland, M.M., C.M. Bitz, and B. Tremblay (2006): Future abrupt reductions in the summer Arctic sea ice. Geophys. Res. Lett., 33, L23503, doi:10.1029/2006GL028024.

8 Budikova, D. (2009): Role of Arctic sea ice in global atmospheric circulation: A review. Global Planet. Change, 68(3), 149–163.

9 Francis, J.A., W. Chan, D.J. Leathers, J.R. Miller, and D.E. Veron (2009): Winter Northern Hemisphere weather patterns remember summer Arctic sea-ice extent. Geophys. Res. Lett., 36, L07503, doi:10.1029/2009GL037274.

10 Petoukhov, V., and V. Semenov (2010): A link between reduced Barents-Kara sea ice and cold winter extremes over northern continents. J. Geophys. Res.-Atmos., ISSN 0148-0227.

11 Seager, R., Y. Kushnir, J. Nakamura, M. Ting, and N. Naik (2010): Northern Hemisphere winter snow anomalies: ENSO, NAO and the winter of 2009/10, Geophys. Res. Lett., 37, L14703, doi:10.1029/2010GL043830.

12 2011 Snow, Water, Ice and Permafrost in the Arctic (SWIPA) assessment - coordinated by AMAP and produced in collaboration with IASC, WMO/Clic and IASSA - Executive Summary (30MB download)

13 Serreze, M. C., A. P. Barrett, and J. J. Cassano (2011), Circulation and surface controls on the lower tropospheric air temperature field of the Arctic, J. Geophys. Res., 116, D07104, doi:10.1029/2010JD015127.

13 Stroeve, J. C., J. Maslanik, M. C. Serreze, I. Rigor, W. Meier, and C. Fowler, 2011. Sea ice response to an extreme negative phase of the Arctic Oscillation during winter 2009/2010, Geophys. Res. Lett., 38, L02502, doi:10.1029/2010GL045662.

14 Inoue, J., and M. Hori (2011) Arctic cyclogenesis at the marginal ice zone: A contributory mechanism for the temperature amplification? Geophys. Res. Lett., doi:10.1029/2011GL047696, in press. [PDF] (accepted 17 May 2011)

15 Overland, J.E., K.R. Wood, and M. Wang (2011): Warm Arctic–cold continents: Impacts of the newly open Arctic Sea. Polar Res., 30, 15787, doi: 10.3402/polar.v30i0.15787. [PDF Version]

16 Jiping Liu, Judith A. Curry, Huijun Wang, Mirong Song, and Radley M. Horton (2012). Impact of declining Arctic sea ice on winter snowfall PNAS 2012 ; published ahead of print February 27, 2012, doi:10.1073/pnas.1114910109

17 Comiso, Josefino C., 2012: Large Decadal Decline of the Arctic Multiyear Ice Cover. J. Climate, 25, 1176–1193. doi: [PDF version]

18 Francis, J. A. and S. J. Vavrus (2012), Evidence linking Arctic amplification to extreme weather in mid-latitudes, Geophys. Res. Lett., 39, L06801, doi:10.1029/2012GL051000.

19 Duarte CM, Lenton TM, Wadhams P, Wassmann P. (2012), Abrupt climate change in the Arctic. Nat Clim Chang. 2011;2:60–62.

20Jeffries, M.O., J.E. Overland, and D.K. Perovich (2013): The Arctic shifts to a new normal. Physics Today, 66(10), 35–40.

21 Overland, J.E., M. Wang, J.E. Walsch, J.C. Stroeve (2013): Future Arctic Climate Changes: Adaptation and Mitigation Timescales. Earth's Future, doi:10.1002/2013EF000162, in press.

22 Overland, J.E., and M. Wang (2013): When will the summer Arctic be nearly sea ice free? Geophys. Res. Lett., 40(10), doi: 10.1002/grl.50316, 2097–2101.