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April 2, 2007 UNIVERSITY OF ALASKA-FAIRBANKS SCIENTIST TO It rides on the ocean, absorbing energy from the circumpolar weather systems. This movement causes a buildup of stress within the ice. Under enough stress, the ice cracks or buckles in a cataclysmic process that resembles the energy released in earthquakes. These continuous ice quakes result in open leads of water or mountainous ridges of broken, jumbled ice. These deformations, in turn, may have an effect on the thickness and durability of the arctic ice pack in the face of climate change. Hutchings, a research associate at the The UAF-led expedition, which also includes lead researchers Cathleen Geiger and Chandra Kambhamettu of the Hutchings said the fieldwork will involve deploying buoys and other instruments to measure the movement and stress of the ice pack in the area around the field camp.
“We are going to use that information to validate the current generation of sea ice models,” Hutchings said. “We are trying to reduce the uncertainty of our prediction of arctic climate change.” Ice deformation may have an effect on climate because open leads of water tend to add more heat and moisture to the atmosphere, which could reduce the overall amount of sea ice. Conversely, if ice movement results in more ridges and thicker ice, the result could be a more durable arctic ice pack that is less vulnerable to seasonal melting. The amount of sea ice is important to the overall understanding of climate change because it is thought to affect how much solar radiation, and hence heat, is reflected back into space. Sea ice is also thought to be an indicator of global temperature changes The expedition also offers scientists a chance to share the field research experience with K-12 students through the National Science Foundation’s PolarTREC program, which links scientists and teachers for collaboration. Robert Harris, a high school teacher from The SEDNA project is funded by a $1.4 million grant from the National Science Foundation. The project will also contribute to the lead International Polar Year project on the state of arctic sea ice.
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