Understanding Ocean Climate
High-resolution computer simulations performed by scientists at the National Oceanography Centre, Southampton (NOCS) are helping to understand the inflow of North Atlantic water to the Arctic Ocean and how this influences ocean climate.
The summer of 2007 saw a record retreat in Arctic sea ice, and in general Arctic climate has become steadily warmer since the early 1990s. This has changed both sea ice drift and upper ocean circulation.
The warm North Atlantic water intrudes into the central Arctic Ocean through Fram Strait, the deep channel between Greenland and Spitsbergen that connects the Nordic Seas to the Arctic Ocean, contributing to sea ice melting.
“We need to understand what is going on because changes in the Arctic Ocean can influence climate around the world,” said Dr Yevgeny Aksenov of NOCS: “The worry is that freshwater from melting ice and increased atmospheric precipitation in the Arctic could ultimately slow the overturning circulation of the North Atlantic, with serious consequences for global climate.”
The researchers used a high-resolution computer model of ocean and sea ice, taking into account the shape of the seabed, and the affects of ice melting, snow and rainfall, solar radiation, and winds. The simulations were verified using long-term measurements of ocean currents and other key climatological and oceanographical data.
“Computers are now powerful enough to run multi-decadal global simulations at high resolution,” said Dr Aksenov: “This helps to understand how the ocean is changing and to plan observational programs so as to make measurements at sea more efficient.”
The researchers find that between 1989 and 2009, about half of the salty North Atlantic water entering the Arctic Ocean came through Fram Strait, and half through the Barents Sea, north of Norway and Russia. However, most of the heat entered the Arctic Ocean through Fram Strait.
Based on their simulations and available observations, they propose a new scheme for the inflow of North Atlantic water into the Arctic Ocean, involving three main routes.
The first delivers warm saline water to the Arctic Ocean through Fram Strait. The other two bring cooled and freshened North Atlantic water to the Arctic Ocean via the Barents Sea.
A northern branch delivers water from the western Barents Sea, mixed to some extent with the Fram Strait branch. Here, North Atlantic water interacts with Arctic waters, resulting in fresh, cold water overlying saltier water below the mixed layer at a depth of around 50-170 meters.
The southern branch supplies the Arctic Ocean with warmer and more saline bottom water formed in the southeastern Barents Sea via full-depth convection and mixing.
Both the northern and southern branches of the Barents Sea flow deliver North Atlantic water to the Arctic Ocean via the 620 meter deep St Anna’s Trough, located east of the Franz Josef archipelago in the far north of Russia. Together they transport around one and a half million cubic meters of water a second.
“Our research is leading to a physically based picture, our eventual goal being a comprehensive understanding of the mechanisms driving ocean climate change,” said Dr Aksenov.
The research was supported by the RAPID Climate Change Program and Arctic Synoptic Basin-wide Oceanography Consortium, Natural Environment Research Council, UK.
The researchers are Yevgeny Aksenov, Sheldon Bacon, Andrew Coward and George Nurser (all of NOCS).
Publication: Aksenov, Y. et al. The North Atlantic inflow to the Arctic Ocean: High-resolution model study. Journal of Marine Systems 79. 1-22 (2010). Published on line in 2009.
Image Caption: This image shows ocean temperature at the 100 m depth and sea ice thickness in Sept. 2006 from the 8 km resolution global model. Credit: NOCS
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