Arctic sea ice

Mitigation has positive environmental impacts

It is widely accepted that the volume of Arctic sea ice has on average been declining over the last thirty years. However, the extent of the sea ice cover in the Arctic remains variable as synoptic weather conditions play a role in determining the growth and melt of sea ice and its movement within the Arctic basin. Arctic sea ice reaches its minimum extent in September and we are currently participating in the Sea Ice Prediction Network (SIPN) international effort to provide a community-wide summary of the expected September mean Arctic sea ice.

International sea ice outlook

The SIPN sea ice outlook includes estimates of September mean sea ice extent from dynamical, statistical and heuristic methods which are combined to provide the median of the estimates. Since 2010, the Met Office has provided an estimate based on our seasonal forecast system. The estimated sea ice extent from the SIPN sea ice outlook for 2010-2014 is shown in the table below:


Outlook median (× 106 km2)

Outlook range (× 106 km2)

Observed (× 106 km2)

Met Office contribution (× 106 km2)

Outlook document





Sea ice outlook 2010 5.5 (PDF, 193 kB)

2010 SEARCH report





Sea ice outlook 2011 4.0 ± 1.2 (PDF, 916 kB)

2011 SEARCH report





Sea ice outlook 2012 4.4 ± 0.9 (PDF, 227 kB)

2012 SEARCH report





Sea ice outlook 2013 3.4 ± 1.5 (PDF, 637 kB)

2013 SEARCH report

2014 (June)

2014 (August)






Sea ice outlook 2014 (Jun) 4.1 ± 1.0 (PDF, 114 kB)

Sea ice outlook 2014 (Aug) 5.3 ± 0.6 (PDF, 107 kB)

2014 SIPN reports

Met Office contribution to the SIPN outlook

Given current capabilities for seasonal forecasting of sea ice, we consider our contribution to the SIPN outlook as an experimental forecast. A prediction of regional-scale ice coverage is beyond the capabilities of current long-range forecasting. Therefore our estimates are restricted to the extent of the Arctic sea ice. This is defined as the area of the Arctic Ocean with at least 15% ice coverage. In the long-term average, this area varies from 14.5-16.5 million km2 in March to 3.5-8 million km2 in September (based on data for 1979-2010). The minimum extent for September since 1979 (the satellite period) was 3.6 million km2 in 2012, almost 20% below the next lowest ice extent of 4.3 million km2 in 2007.

Using retrospective forecasts for the period 1996-2009, we have assessed the skill of the current prediction system. Over this verification period, the correlation between our forecast September Arctic ice extents and the observed ice extents is 0.87. This is significantly different from zero at the 95% confidence level. However, it is not significantly better then predictions made by a simple extrapolation of the observed trend. Shown below are our forecast ice extents (green diamonds) compared to the observed ice extents during this period (black squares). The dashed black line is the observed trend in the ice extent over the 1996-2013 period, while the green dashed line (barely distinguishable from the black dashed line on the graph) is the trend produced by the forecast system. The 2013 value is obtained using the GloSea5 seasonal forecast system.

sea ice predictions Aug 2014 September sea ice extent forecasts (green) and observations (black)

Last updated: 5 March 2015