New Book Co-Edited by U of A Geoscientist Examines Cold Environments

John C. Dixon, University of Arkansas, and the cover of his book.
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John C. Dixon, University of Arkansas, and the cover of his book.

FAYETTEVILLE, Ark. – A new book co-edited by a University of Arkansas geoscientist describes the diversity of artic and alpine climates, and how they are susceptible to climate change.

The book, Source-to-Sink Fluxes in Undisturbed Cold Environments, provides an overview of the latest research of the working group of the International Association of Geomorphologists, said John C. Dixon, professor in the Department of Geosciences in the J. William Fulbright College of Arts and Sciences.

Forty-four scientists worldwide contributed to the book, which includes case studies covering arctic, Antarctic and alpine environments.

“We identify the main factors accounting for differences in the amounts of solid and dissolved materials transported across cold climate landscapes,” Dixon said. “We also explain why there are variations in the amounts of solid and dissolved materials transported in different cold climate landscapes. This research has particular implications for water quality and nutrient availability in these ecologically sensitive environments.”

Over the past 12 years, the working group has been observing the presence and availability of ice and running water in the fall season – and also the availability of ground ice for moving surface materials around through freezing and thawing – at 36 test sites around the world.

The focus of the research has been to better understand the ways in which climate change in these sensitive environments are likely to impact the magnitude and frequency of landscape change, he said.

“We are seeing a window to what will happen less intensely at lower latitudes,” he said.

The book stresses that cold climates are not uniform in their appearance and in the processes that operate within them, Dixon said. There is much greater variability in alpine landscapes than other cold climates, for example.

“This is a reflection of things like the bedrock that dominates, the aspect of the valley, the amount of vegetation cover or surface debris,” he said. “All of these variables influence the rate at which materials are moved around on the Earth’s surface.”

Dixon co-edited the book with Achim A. Beylich of the Geological Survey of Norway and Zbigniew Zwolinski of the Institute of Geoecology and Geoinformation at Adam Mickiewicz University in Poland.

Source-to-Sink Fluxes in Undisturbed Cold Environments is published by Cambridge University Press.

Contacts

John C. Dixon, professor
Department of Geosciences
479-575-5808, jcdixon@uark.edu

Chris Branam, research communications writer/editor
University Relations
479-575-4737, cwbranam@uark.edu


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