A paper recently published in Science Advances has revealed, for the first time, the impact of underwater tsunamis in Antarctica on the mixing of the ocean.
The study, led by the British Antarctic Survey (BAS) and co-authored by scientists including the National Oceanography Centre’s (NOC) Dr Filipa Carvalho, improves knowledge on what these tsunamis mean for the climate, ecosystem and sea level rise.
Scientists on a research vessel in Antarctica watched the front of a glacier disintegrate and their measurements ‘went off the scale’. As well as witnessing disruptions on the ocean surface, scientists recorded ‘internal’ underwater tsunamis as tall as a house, a phenomenon that has been previously missed in the understanding of ocean mixing and in computer models.
Internal tsunamis are an important factor in ocean mixing, affects life in the ocean, temperatures at different depths, and how much ice the ocean can melt.
How glaciers calve
Ice in Antarctica flows to the coast along glacier-filled valleys. While some ice melts into the ocean, a lot breaks off into icebergs, which range in size from small chunks up to the size of a country. A team on board the British Antarctic Survey (BAS) research ship RRS James Clark Ross were taking ocean measurements close to the William Glacier, situated on the Antarctic Peninsula, as the front of it dramatically disintegrated into thousands of small pieces.
The William Glacier typically has one or two large calving events per year, and the team estimated this one broke off around 78,000 square metres of ice – around the area of ten football pitches – with the front of the glacier towering 40m above sea level. Before it broke away, the water temperature was cooler at around 50–100m in depth and warmer below this. After the calving, this changed dramatically, with temperature much more even across different depths.
Lead author of the study Professor Michael Meredith, who’s head of the Polar Oceans team at BAS, was there. He says: “This was remarkable to see, and we were lucky to be in the right place at the right time. Lots of glaciers end in the sea, and their ends regularly split off into icebergs. This can cause big waves at the surface but we know now it also creates waves inside the ocean. When they break, these internal waves cause the sea to mix and this affects life in the sea, how warm it is at different depths and how much ice it can melt.
“This is important for us to understand better. Ocean mixing influences where nutrients are in the water and that matters for ecosystems and biodiversity. We thought we knew what caused this mixing – in summer, we thought it was mainly wind and tides, but it never occurred to us that iceberg calving could cause internal tsunamis that would mix things up so substantially.”
As opposed to the waves caused by wind and tides, tsunamis are caused by geophysical events where water is suddenly shifted, for example by an earthquake or landslide. Internal tsunamis have been noticed in a handful of places, caused by landslides. Until now, no one had noticed that they are happening around Antarctica, probably all the time because of the thousands of calving glaciers there. Other places with glaciers are likely affected also, including Greenland and elsewhere in the Arctic.
This chance observation and understanding is important, as glaciers are set to retreat and calve more as global warming continues. This could likely increase the number of internal tsunamis created and the mixing they cause.
This process is not factored into current computer models enabling us to predict what might happen around Antarctica. This discovery changes our understanding of how the ocean around Antarctica is mixed and will improve knowledge about what it means for climate, the ecosystem and sea level rise.
Michael Meredith continues “Our fortuitous timing shows how much more we need to learn about these remote environments and how they matter for our planet.”
More data is needed
NOC Oceanographer Dr Filipa Carvalho discussed the biogeochemical implications in the study: “As a biological oceanographer, it was really exciting to look at the biogeochemical data before and after the calving event. It was striking to see how much mixing occurred across the bio-optical and nutrient data. Although there weren’t enough data to fully quantify the effect from a biogeochemical perspective – this was a fortunate being at the right place at the right time event, we now know it has the potential to be very important for primary production and consequent carbon sequestration. We need to investigate this further, and with the help of autonomous platforms fitted with biogeochemical sensors, collect targeted data at these important sites. This will help us to really understand the implications of such events have on ocean biogeochemistry and the overall climate in a key region such as Antarctica.”
The research cruise on RRS James Clark Ross was part of the ICEBERGS project and was funded by the Natural Environment Research Council.