A porthole on the ocean – episode 1: Coccolithophores
Climb aboard the schooner Tara and discover the secret world of coccolithophores What are coccolithophores? What do they look like? Why are they so important for us?
Support our mission
Make a donationA high-risk 18-month expedition drifting with the sea ice on the edge of the North Pole to see the effects of climate change.
In brief
Although the schooner was originally designed for this polar drift by architects Olivier Petit, Luc Bouvet and engineer Michel Franco, we never got the chance to test the accuracy of the calculations against the many assaults of the sea ice. The first time was a moment of truth…
Setting sail in May 2006 from Lorient, its home port, the schooner Tara and its crew embarked on a human adventure as risky and unprecedented as that of Fridtjof Nansen’s Fram more than a century earlier. The International Polar Year 2007-08 was an opportunity to invest in polar research, a true watchdog for future climate change. For nearly 500 days, or two nights and one polar day of six months each, in temperatures of -25°C, the schooner drifted across the Arctic Ocean with the ice floe. At an average speed of 10 km per day, the eleven men and women furthest north of humanity took readings and measurements from a depth of 3,500 m to an altitude of 2,000 m with the aim of feeding the IPCC models to try to predict major climatic events in Europe.
Why is the sea ice disappearing so rapidly?
What are the dynamics of the annual melt according to the seasons?
To convince people of the urgency through a unique and original human adventure at the cutting edge of the collective climatic understanding.
To be able to predict major climatic events in Europe.
To be there with time
The fact that we had been on the ice, in the ice and with the ice for over a year, enabled us to put our finger on the major aspects of its seasonal cycle via new simultaneous surveys of the three elements which are the atmosphere, the ocean and the sea ice.
The importance of the albedo
We were also able to understand the effects of the albedo, that fraction of solar energy reflected into space, compared to other oceanic and atmospheric phenomena which transfer a large amount of heat from the equator towards the poles, both in summer and in winter.
Lack of cold in winter
We also noticed that the ice was weakened much more in winter. Of course, the melting process takes place in summer, but the massive retreats of ice that we observe are much more associated with the processes of winter. Because winters are much less harsh than before, less cold produces less ice which melts more easily with the return of the summer sun.
Actualités