Warming Ocean Contributes to Global Warming

The warming of an Arctic current over the last 30 years has triggered the release of methane, broken down from methane hydrate stored in the sediment beneath the seabed. Scientists at the University of Birmingham, working in collaboration with researchers from the National Oceanography Centre Southampton, Royal Holloway London and IFM-Geomar in Germany have found that more than 250 plumes of bubbles of methane gas are rising from the seabed of the West Spitsbergen continental margin in the Arctic, in a depth range of 150 to 400 metres. Methane released from gas hydrate in submarine sediments has been identified in the past as an agent of climate change. The likelihood of methane being released in this way has been widely predicted. The data was acquired from the research ship RRS James Clark Ross, as part of the Natural Environment Research Council's Arctic Initiative. The bubble plumes were detected using sonar and then sampled with a water-bottle sampling system over a range of depths. Graham Westbrook, Professor of Geophysics at the University of Birmingham, says: "It appears that the warming of the northward-flowing West Spitsbergen current by 1° over the last thirty years has caused the release of methane by breaking down methane hydrate in the sediment beneath the seabed." Methane hydrate is an ice-like substance composed of water and methane which is stable in conditions of high pressure and low temperature.