The Ross Ice Shelf is the largest on the planet at 480,000 square kilometres. It is many hundred metres thick and more than 600km wide.
Dr Stevens conducted the ocean measurements during an expedition in December 2017 when a hot water drill bored 350m metres through the ice to the ocean below. Instruments were then lowered through the hole and left for two years to record ocean currents and water temperature with data transmitted via satellite.Securing the measurements underneath hundreds of metres of ice 350km from Scott Base presented a massive challenge for scientists, but Dr Stevens says the information gathered emphasises the importance of carrying out these kinds of expeditions. Importantly it was a highly collaborative science expedition. It was led by the University of Otago and the drill team came from Victoria University of Wellington and demonstrated how scientists from CRIs and universities collaborate.
The fiery orange submarine, which she named Ran after the Norse goddess of the sea, hadn’t yet resurfaced from its first mission in the watery depths around the face of West Antarctica’s Thwaites Glacier.“She’s a very temperamental lady,” Wåhlin said of the $3.6 million, unmanned submarine, while peering through her binoculars on an overcast March day.
“Future climate projections largely depend on the longevity of the ice shelves so it is important to see what has changed. Bringing together observed and modelled perspectives is critical for improving our predictions of ice sheet evolution and how that will impact the planet.”
He says the data collected, and comparisons with the 1977 data, provide valuable insight into the how the ocean circulates in the cavity under the ice shelf and the complexity of the processes involved.
Some key differences were observed between the measurements and those taken 40 years ago including salinity which reflects continent-wide changes. The team also observed short-term re-freezing on the underside of the ice shelf which Dr Stevens says has implications for the melt rate and the dynamics of the upper ocean.
“This new insight emphasises the importance of making these observations in the environment where they are taking place. These virtually unexplored areas are hidden from the sun and wind by hundreds of metres of ice and are subject to processes that we are not used to seeing in the open ocean.”
The next phase will explore how to integrate these new measurements into the climate models.
The research was facilitated by the New Zealand Antarctic Research Institute (NZARI) funded Aotearoa New Zealand Ross Ice Shelf Programme, the Victoria University of Wellington Hot Water Drilling initiative and Antarctica New Zealand.
“We have dramatically lifted the amount of data available and provided a basis for better understanding the complex processes that drive melting.”