These spectacular outburst floods happen as dams of ice and earth give way or, as from Vatnajokull in Iceland in 1996, when a volcano erupts beneath a glacier. That outburst flood was 10km wide, swept away a bridge and left behind icebergs 10m high.
For the first time, scientists can model the impact of these floods, the damage they could cause and the changes they will make to the landscape. Improved computer power allows them to take digital maps of an area metre by metre and picture the impact of the water as well as the materials carried by the flood.
The power of jokulhlaups means that it's not possible to take conventional measurements of flow and the sediment load. Instead Leeds researcher and School of Geography lecturer Dr Jonathan Carrivick and colleagues have used geological detective work to examine the landscape created by a flood and calculate the energy and mechanisms needed to generate these shapes.
Outburst floods can pose a major hazard in mountainous areas. Dr Carrivick said: "It's the rocks, sediment and ice which do most damage and create the most impressive landforms not just the water, and it's only now that we can model the impact of the load of these floods."
"This is really important for hazard management and also because flood size and frequencies will alter with climate change. In particular, global warming will lead to changes in how fast glaciers melt, and the mode by which meltwater is released."
Dr Carrivick is waiting for a jokulhlaup in New Zealand this summer. The Mount Ruapehu area has been set-up for measurements by local researchers and the existing landscape mapped at very high resolution. It's hoped that the before and after maps - as well as some measurements of the flood - will support his model.
For more information, contact:
Hannah Love, press office, University of Leeds, 0113 343 4100, 07974 184542, email@example.com Dr Jonathan Carrivick, School of Geography, University of Leeds [in Iceland] via J.L.Carrivick@leeds.ac.uk or the University press office can get a message to Dr Carrivick through the the symposium organisers.
Note to editors:
Dr Carrivick presents his paper 'Modelling transient hydrodynamics and rapid landscape change due to a high-magnitude outburst flood: and example from Kverkfjoll volcano, Iceland' at 4.30pm on Friday 23 June 2006 at the International Glaciological Society's International Symposium on Earth and Planetary Ice-Volcano Interactions in Reykjavík, Iceland.
More about Dr Carrivick is online at: http://www.