Captain Scott’s expedition logs reveal Antarctic sea ice history
Data gaps
If we take just the satellite record, which began in 1979, Antarctica’s sea ice has shown a small but steady increase. Over in the northern hemisphere, meanwhile, Arctic sea ice has declined rapidly over the same period. The reasons for the contrasting fortunes of sea ice at the Earth’s poles has prompted a lot of speculation in the media and by scientists. A recent study, for example, pinpointed a natural shift in the Pacific Ocean as a key factor in a growth spurt of Antarctic sea ice between 2000 and 2014. One of the limitations to understanding exactly how and why Antarctic sea ice is changing is the relatively short length of satellite data records, says Dr Jonathan Day, co-author of the new study published in The Cryosphere. He explains to Carbon Brief:“Relatively little is known about the state of Antarctic sea ice before continuous satellite records began in the 1970s, making it hard to understand if [the increase] is a trend.”
Day’s study helps to fill in this data gap using ship logbooks kept by Antarctic explorers during the Heroic Age of Antarctic Exploration between 1897 and 1917. As part of these missions, scientists recorded the position and state of the sea ice in ships’ logbooks, explains Day:“These records were very diligently kept by trained meteorologists onboard ship, so the quality of the record keeping is high.”
![Photograph entitled: 'With Captain Scott [Royal Navy] to the South Pole (British Antarctic Expedition)'. Steam Yacht 'Terra Nova' with dogs and men standing on ice near by', by Herbert Ponting (1870-1935)](https://www.carbonbrief.org/wp-content/uploads/2016/11/Steam_Yacht_Terra_Nova.jpg)
‘Surprisingly comparable’
The researchers digitised the logbooks from 11 expeditions and added the data by hand into spreadsheets. They were helped by various other research groups as part of the International Comprehensive Ocean-Atmosphere Data Set (ICOADS), a worldwide effort to recover weather data from ships’ logbooks. You can see the routes that the explorers took in the map below.
Preserving old records
While a 14% loss is not an insignificant amount, it’s smaller than some of the changes in Antarctic sea ice recorded during the middle of the 20th century, as estimated from whaling ship logbooks, the paper says. The findings suggest that Antarctic sea ice has fluctuated substantially through the last century, rather than experiencing the sort of steady trend seen in the Arctic over many decades. This indicates that summer sea ice in the Antarctic is heavily influenced by natural fluctuations in the climate system, which can mask the impact of human-caused climate change, says Day:“What this study shows is that summer sea ice in the Antarctic might not be particularly sensitive to a warming climate compared to the Arctic, however it does leave open the possibility that there has been a decrease in ice extent of at most 14%.”
Day discusses his study in the video below. The study highlights what’s happening to sea ice can be quite different in each of the Earth’s poles, says Florence Fetterer, principal investigator at the National Snow and Ice Data Centre (NSIDC), who wasn’t involved in the study, but peer-reviewed the paper. She tells Carbon Brief:“The study reinforces the idea that looking at Arctic and Antarctic ice separately is the best way to understand decadal and long-term trends, because it suggests significant decadal and inter-decadal variability in southern hemisphere ice extent going back much further than the last 30 years.”
Fetterer – who recently wrote a guest article for Carbon Brief on piecing together a record of Arctic sea ice back to 1850 – also says the study highlights how important it is to find and preserve old observations:“I hope it will bring attention to international projects like Old Weather that are working to ensure that the observations are not lost.”
Article information
Edinburgh, T. & Day, J. (2016) Estimating the extent of Antarctic summer sea ice during the Heroic Age of Exploration, The Cryosphere, doi:10.5194/tc-10-2721-2016.