Phosphorus is a key nutrient that could, if it reaches the open ocean, enrich waters of the Arctic Ocean, potentially stimulating growth of the marine food chain.
Phosphorus feeds plankton at the base of the ocean food web. Glacial meltwater has long been known to contain phosphorus, but new research by Dr Jon Hawkings, from the Cabot Institute at the University of Bristol, shows as the Greenland ice sheet melts, it could be releasing far more of the nutrient than previously thought..
Dr Hawkings and his collaborators spent three months in 2012 and 2013 gathering water samples and measuring the flow of water from the 600-square-kilometer (230-square-mile) Leverett Glacier, and the smaller, 36-square-kilometer (14-square-mile) Kiattuut Sermiat Glacier in Greenland, as part of a Natural Environment Research Council-funded project to understand how much phosphorus, in its various forms, was escaping from the ice sheet over time and draining into the sea. They used that data to extrapolate how much phosphorus was likely being released from the entire Greenland ice sheet.
'We found greater amounts of phosphorus in the waters of the Leverett Glacier than had been detected at previous study sites, which have looked mostly at smaller glaciers. The large Leverett Glacier, however, is more representative of the glaciers that contribute the bulk of meltwater coming from the Greenland ice sheet,' said Dr Hawkings.
The team found annual phosphorus input (for all of Greenland's outlet glaciers) is at least equal to some of the world's largest rivers, such as the Mississippi and the Amazon. That amount could increase as the climate warms and more ice melts. The report on their findings has been accepted for publication in Global Biogeochemical Cycles, a journal of the American Geophysical Union.
Dr Hawkings said: 'It is not clear yet how much of the phosphorus being released from the ice sheet is reaching the open ocean, but if a large amount of phosphorus coming off the glacier makes it to the sea, the nutrient could rev up biological activity of Arctic waters.
'It could stimulate growth of plankton at the base of the ocean food web, which could impact birds, fish and marine mammals higher up the food chain. The research also suggests ice sheet-derived phosphorus could eventually reach the northern Pacific and Atlantic oceans, which are connected to the Arctic Ocean.'
Oceanographers have historically thought of glaciers and ice sheets as frozen systems that don't add nutrients or water to the oceans, Dr Hawkings explained. Research over the past couple of decades has shown there is flowing water at the base of glaciers. As climate change warms Greenland, and more ice melts and makes its way into the sea, the ice sheet is potentially becoming a more important source of nutrients.
'Glacial meltwater gains phosphorus when it travels in moulins, or pipes in the ice - through the guts of the glacier and down to the where the ice meets the bedrock.
'Where the ice meets the bedrock at the very bottom of the glacier, the meltwater is exposed to phosphorus-rich rocks that are pulverized by the moving glacier. Glaciers are very, very good at crushing up rock," said Dr Hawkings.
The concentrations of dissolved phosphate the researchers found in the Leverett Glacier meltwater - which is just one form of phosphorus found in the meltwater - were similar to concentrations found in Arctic rivers, and among the highest levels recorded in glacial meltwaters worldwide. The total phosphorus concentrations found in the meltwater of the Leverett glacier - which includes phosphorus-rich particles - was 10 times greater than concentrations found in Arctic river waters.
If the majority of the phosphorus found in meltwater from all of Greenland's glaciers reaches the sea, it would be equal to about 400,000 metric tons (440,000 U.S. tons) per year of phosphorus, more than Arctic rivers are estimated to contribute to the Arctic Ocean, according to the new study. However, how much phosphorus makes it from the meltwater into the open oceans is not yet known. Dr Hawkings noted that the largest portion of phosphorus, which is in the form of powdered rock minerals, could be settling out of the meltwater and ending up buried in Greenland's fjords before it has time to dissolve.
"This is an important finding because it highlights the role that the rapidly changing Greenland ice sheet plays in supplying nutrients to the Arctic Ocean," said Dr Eran Hood, of the University of Alaska Southeast in Juneau, who studies the meltwater from coastal glaciers in Alaska, and was not involved in the new study.
'Now we need to understand how much of this phosphorus, especially in the particulate form, ends up being utilized in high-latitude marine ecosystems," said Hood. "I think that's an important open question."
Hawkings, J., Wadham, J., Tranter, M., Telling, J., Bagshaw, E., Beaton, A., Simmons, S., Chandler, D., Tedstone, A., Nienow, P. (2016) "The Greenland Ice Sheet as a hotspot of phosphorus weathering and export in the Arctic", Global Biogeochemical Cycles, doi: 10.1002/2015GB005237
To arrange an interview with Dr Hawkings, contact the press office at the University of Bristol on +44 (0)117 331 8092
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The Cabot Institute carries out fundamental and responsive research on risks and uncertainties in a changing environment. We drive new research in the interconnected areas of climate change, natural hazards, water and food security, low carbon energy, and future cities. Our research fuses rigorous statistical and numerical modelling with a deep understanding of social, environmental and engineered systems - past, present and future.
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Global Biogeochemical Cycles