- Giant icebergs leave trail of carbon sequestration in their wake -- a month after they have passed
- Geographers analysed 175 satellite images of ocean colour which is an indicator of phytoplankton productivity at the ocean's surface Giant icebergs are responsible for storing up to 20 per cent of carbon in the Southern Ocean, a new study has found.
Pioneering research from the University of Sheffield's Department of Geography discovered melting water from giant icebergs, which contains iron and other nutrients, supports hitherto unexpectedly high levels of phytoplankton growth.
This activity, known as carbon sequestration, contributes to the long-term storage of atmospheric carbon dioxide, therefore helping to slow global warming.
During the study, which is the first of its kind on this scale, a team of scientists led by Professor Grant Bigg analysed 175 satellite images of ocean colour -- which is an indicator of phytoplankton productivity at the ocean's surface -- from a range of icebergs in the Southern Ocean which were at least 18 km in length.
The images from 2003-2013 showed that enhanced phytoplankton productivity, which has a direct impact on carbon storage in the ocean, extends hundreds of kilometres from giant icebergs, and persists for at least one month after the iceberg passes.
Professor Bigg said: "This new analysis reveals that giant icebergs may play a major role in the Southern Ocean carbon cycle.
"We detected substantially enhanced chlorophyll levels, typically over a radius of at least four-10 times the iceberg's length.
"The evidence suggests that assuming carbon export increases by a factor of five-10 over the area of influence and up to a fifth of the Southern Ocean's downward carbon flux originates with giant iceberg fertilisation.
"If giant iceberg calving increases this century as expected, this negative feedback on the carbon cycle may become more important than we previously thought."
The Southern Ocean plays a significant part in the global carbon cycle, and is responsible for approximately 10 per cent of the ocean's total carbon sequestration through a mixture of biologically driven and chemical processes, including phytoplankton growth.
Previous studies have suggested that ocean fertilization from icebergs makes relatively minor contributions to phytoplankton uptake of CO2.
However this research, published today (Jan. 11, 2016) in Nature Geoscience, shows that melting water from icebergs is responsible for as much as 20 per cent of the carbon sequestered to the depths of the Southern Ocean.
Notes to Editors
University of Sheffield
With almost 26,000 of the brightest students from around 120 countries, learning alongside over 1,200 of the best academics from across the globe, the University of Sheffield is one of the world's leading universities. A member of the UK's prestigious Russell Group of leading research-led institutions, Sheffield offers world-class teaching and research excellence across a wide range of disciplines. Unified by the power of discovery and understanding, staff and students at the university are committed to finding new ways to transform the world we live in. In 2014 it was voted the number one university in the UK for Student Experience by Times Higher Education and in the last decade has won four Queen's Anniversary Prizes in recognition of the outstanding contribution to the United Kingdom's intellectual, economic, cultural and social life. Sheffield has five Nobel Prize winners among former staff and students and its alumni go on to hold positions of great responsibility and influence all over the world, making significant contributions in their chosen fields. Global research partners and clients include Boeing, Rolls-Royce, Unilever, AstraZeneca, Glaxo SmithKline, Siemens and Airbus, as well as many UK and overseas government agencies and charitable foundations.
For further information, please visit http://www.
For further information please contact:
Media Relations Officer
University of Sheffield
To read other news releases about the University of Sheffield, visit http://www.