Guest post: Piecing together the Arctic’s sea ice history back to 1850

11.08.16

Arctic

By:

Florence Fetterer

A guest article by Florence Fetterer, principal investigator at the National Snow and Ice Data Centre (NSIDC) in the US. Sea ice cover in the Arctic has undergone a widely reported decline in recent decades. The decrease has been greatest during summer, with sea ice extent reducing by around 12% per decade since the satellite record began in 1979. The main cause of this rapid decline is rising air temperatures. The Arctic is warming twice as quickly as the global average, a phenomenon known as Arctic amplification. Other factors, such as wind patterns and ocean warming, also play a role in the diminishing sea ice.

Satellites provide a near-continuous record of Arctic sea ice cover, allowing scientists to monitor changes from one day to the next. But because this data spans only the most recent three and a half decades, we need to look elsewhere to gather information on variations over longer periods. This data is necessary as there are some research questions that can’t be answered with only short-term records, such as:

1. Has Arctic sea ice cover been this small since the start of the industrial revolution?
2. Has sea ice ever declined this rapidly in the historical record?
3. How is sea ice affected by natural fluctuations over multiple decades?

To tackle this problem we set about constructing a record of sea ice going back to 1850. And this meant gathering data from some rather unusual sources.

Digitising data

First, a little background. In the 1970s, the world’s community of sea ice researchers was a small one. Academics were mainly interested in the role sea ice played in regulating the surface energy balance of the Arctic. Sea ice insulates the cold atmosphere from the warmer ocean, reflects sunlight throughout the polar summer, and releases or stores heat through the process of melting or freezing. At the time, the question of whether variability in Arctic sea ice extent was being affected by the climate was still an open one. Nevertheless, scientists were still concerned about preserving existing data on sea ice, and gathering more, with the aim of producing an Arctic-wide view of sea ice conditions. Observations of sea ice came from far and wide, including ship reports, aeroplane surveys, compilations by naval oceanographers, and analyses by national ice services and meteorological offices. Prof John Walsh, now at the University of Alaska Fairbanks, and Dr Mick Kelly, from the University of East Anglia (now retired), were pioneers at retrieving data. They hand-digitised information from sources, such as aerial surveys, from the US Navy and UK Meteorological Office, and from the Danish Meteorological Institute’s yearbook maps (see examples from 1978 and 1979 – both pdfs). Walsh, along with Prof William Chapman from University of Illinois, used these various sources to make monthly grids in Arctic and Southern Ocean sea ice concentrations, covering the period 1901-95. These grids proved to be very popular among researchers – possibly because there were few alternatives. However, the early years of this record had significant gaps. Almost no ice information was collected during the second world war, for example. These gaps were filled by using the long-term averages for each month. This is illustrated in the charts below, which show monthly sea ice data from the Met Office Hadley Centre (red and black lines) and the recent NASA satellite record (blue line).

While this data provides an indication of long-term sea ice changes, it doesn’t accurately reflect the ups and downs of natural variability. This presents a problem for climate modellers, who need data with realistic past sea ice fluctuations on which to base their projections for the future. Fortunately, in the decade since those monthly grids were published, more historical data sources have become available.

New sources

We’ve used a range of new data sources to fill gaps and extend the Arctic sea ice record back to 1850. We’ve also updated the record with the latest satellite data. These are some of the sources of information we used to create our sea ice dataset:

• The sea ice edge positions in the North Atlantic, between 1850 and 1978, derived from various sources, including newspapers, ship observations, aircraft observations, diaries and more.
• Sea ice concentration data from regular aerial surveys of ice in the eastern Arctic by the Arctic and Antarctic Research Institute, St. Petersburg, Russia, beginning in 1933.
• Sea ice edge positions for Newfoundland and the Canadian Maritime Region from observations, for 1870 to 1962.
• Detailed charts of ice in the waters around Alaska for 1954 to 1978, originally the property of a consulting firm (the Dehn collection).
• Arctic-wide maps of ice cover from the Danish Meteorological Institute from 1901 to 1956.
• Whaling ship logbook entries that noted ship position along with an indication of whether the ship was in the presence of ice (see image of whaling ship below).

These new sources already existed as data compilations in one form or another before we got hold of them. But many needed digitisation and interpretation before the information could be incorporated into a long-term record. For example, below is one of the aerial survey maps from the Arctic and Antarctic Research Institute in Russia. The different colour shading indicates the coverage of sea ice.

You can see another source of data below, this time one of the maps from the Danish Meteorological Institute. These are remarkable for their information value and because they represent a cooperative international effort to report ice conditions in a systematic way that was sustained over decades. The red symbols and terms in the legend (see close-up below the map) indicate the sea ice extent. “Tight pack-ice”, for example, indicates ice of 70% to 90% concentration of ice over the sea.

The result of all this work is our new dataset, “Gridded Monthly Sea Ice Extent and Concentration, 1850 Onwards”. This has a much more realistic representation of the year-to-year fluctuations in sea ice, as well as the long-term trend. The charts below illustrate the new record. The blue line shows Arctic sea ice extent in March, at the end of the winter when the ice is at its annual maximum. The red line shows sea ice cover in September, at the end of the summer when ice extent shrinks to its yearly minimum.

Most fundamentally of all, the new dataset allows us to answer the three questions we posed at the beginning of this article. First, there is no point in the past 150 years where sea ice extent is as small as it has been in recent years. Second, the rate of sea ice retreat in recent years is also unprecedented in the historical record. And, third, the natural fluctuations in sea ice over multiple decades are generally smaller than the year-to-year variability.