Retreat of Arctic sea-ice: A scientific perspective

Retreat of Arctic sea-ice: A scientific perspective

 

Jeremy Wilkinson, ICE-ARC Programme Coordinator, British Antarctic Survey

 

The retreat of summer Arctic sea ice is unquestionable.  The use of the word unquestionable is deliberate as for over 35 years special satellite-mounted sensors, which can see through cloud and the polar night, have been continuously obtaining daily ‘images’ of the entire Arctic region.  From these Arctic-wide images, the extent of the sea ice can be clearly and accurately determined, day after day and year after year.  The resultant time-series shows that we have moved from an average sea ice extent in September of over 7 million km2 in the 1970s to about 3.5 million km2 in 2012; a loss of about half the summer Arctic sea ice cover.  It is important to note that this reduction is not expected to be consistent from one year to the next. For example, a year with smaller ice extent could be followed by a number of years with a significantly larger ice extent. This is Mother Nature in action, and variability is fully expected.  With this in mind, the increase in ice extent over the last two years (since the 2012 minimum) is neither unusual nor unexpected.  It is the trend (the change over the entire time-series) that is significant; which unquestionably shows a substantial decrease over the time-series (see figure).  Importantly, all climate models predict that the extent of the summer Arctic sea ice will continue to retreat over the coming decades; none show an increase.

Arctic sea-ice extend to Sept 2013

Arctic sea-ice extent has been in decline since the satellite era, as shown here for the month of September.  The black line shows the average sea-ice extent for September for the years 1978 to 2013 as seen by space-based measurements.  The blue line displays the best linear fit to data. Year-to-year variability about the overall decline in sea-ice extent is also evident. (Credit: NSIDC)

 

Background

We have witnessed changes to the Arctic system that only a decade ago would not have been thought possible. These changes have the potential, through complex linkages and feedback mechanisms, to influence all aspects of the Earth system.  As a consequence, Arctic change will have a significant impact on the livelihoods of Arctic residents, as well as considerable socio-economic implications at national, regional, and global levels.  Whether their net impact is positive or negative is still open to debate.  For example, observed changes have already led to greater marine access to previously ice-covered waters and, as a result, we have witnessed an intensification of activities such as fishing, oil and mineral exploration/exploitation, shipping, and tourism.  These short-term gains may be offset by the long-term impact of global warming through our increased susceptibility to high-cost natural events such as severe storms, sea-level rise, and extensive species loss.  Given the global consequences of Arctic change we have to ensure that public, industry, national and international politicians and policy-makers have the most up-to-date and robust science available on Arctic change. Good policy decisions are based on rigorous scientific analysis.  The recent controversy regarding the “increase” in the Arctic summer sea-ice extent over the past two summers needs to be placed in context within the time-series available.

 

The Arctic is changing and will continue to change.  It is clear that we need to better understand Arctic change. This is an exceedingly difficult task as the issues associated with Arctic change transcend national boundaries, sectors, and disciplines. No one nation has the sovereignty, expertise, or budget to individually tackle these challenges head on; a truly international and integrated scientific effort is needed.  Through international programmes like the EU-funded ICE-ARC we are developing a better understanding of the fundamental workings of the Arctic system, and the net consequences of these changes to the global economy.

 

Notes

 

What is the ‘Arctic sea-ice minimum’?

The Arctic is an ocean surrounded by land and Arctic sea ice is the thin layer of frozen ocean water that forms and grows during the winter, and melts in the summer. The Arctic sea-ice minimum marks the day – typically in September – when sea ice reaches its smallest extent at the end of the summer melt season.

 

Is sea ice also decreasing in the Antarctic?

Since 1979 Antarctic sea ice extent has increased throughout the year, with the total Antarctic annual mean sea-ice extent having increased at a rate of 1.5% per decade. However, this overall increase masks large regional variations around the continent, and especially an increase over the Ross Sea and a decrease over the Amundsen-Bellingshausen Sea. The mechanism or mechanisms responsible for the increase in Antarctic sea-ice extent are not fully understood, but the loss of stratospheric ozone, freshwater injection from the ice sheet, ocean-ice feedback processe, and ocean change have all been put forward as possibly playing a part. However, the overall sea ice increase around Antarctica’s coastline may be within the bounds of internal variability of the climate system.

 

Is sea ice decreasing globally?

Yes, although the area of Antarctic sea ice has increased slightly in recent years, the loss in total area of sea ice in the Arctic outweighs that considerably. On average Arctic sea ice has reduced by approximately 3.5 million km² in the past 35 years, whereas Antarctic sea ice has increased by around 0.5 million km² in the same time period. So, overall the world has lost approximately 3 million km² in the past 35 years.

 

Glossary

 

Sea ice is the thin layer of frozen ocean water that forms and grows during the winter, and melts in the summer.

Sea-ice extent is the area of ocean covered by sea ice covering extensive regions of the world, most notably in Antarctica and Greenland.

Ice sheets are formed from snow that falls on land creating thick layers of ice.

Ice shelves are the floating extensions of grounded ice – they can be hundreds of metres thick, while sea ice is only a few metres thick.

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Last updated on 11-11-2017 17:34