The Arctic Hydrologic System in Transition: A Heuristic Look at This Dynamic Environment
Jennifer A. Francis1, Daniel M. White2, John J. Cassano3, William J. Gutowski, Jr.4, Larry D. Hinzman5, Marika M. Holland6, Michael A. Steele7, Charles J. Vörösmarty8
1Institute of Marine and Coastal Sciences, Rutgers University, New Brunswick, NJ, USA, jenniferafrancis [at] yahoo [dot] com
2Institute of Northern Engineering, Fairbanks, AK, USA, dmwhite [at] alaska [dot] edu
3Department of Atmospheric and Oceanic Sciences, Boulder, CO, USA, john [dot] cassano [at] colorado [dot] edu
4Department of Geological and Atmospheric Sciences, Iowa State University, Ames, IA, USA, gutowski [at] iastate [dot] edu
5International Arctic Research Center, University of Alaska Fairbanks, Fairbanks, AK, USA, lhinzman [at] iarc [dot] uaf [dot] edu
6National Center for Atmospheric Research, Boulder, CO, USA, mholland [at] ucar [dot] edu
7Polar Science Center, Applied Physics Laboratory, University of Washington, Seattle, WA, USA, mas [at] apl [dot] washington [dot] edu
8Department of Civil Engineering, City College of New York, New York, NY, USA, cvorosmarty [at] ccny [dot] cuny [dot] edu
In this presentation we will explore the article recently published by Francis et al. (2009) providing a heuristic approach to change in the arctic hydrologic system.
The pace of change in the arctic system during recent decades has captured the world's attention. Observations and model simulations both indicate that the arctic experiences an amplified response to climate forcing relative to that at lower latitudes. At the core of these changes is the arctic hydrologic system which includes ice, gaseous vapor in the atmosphere, liquid water in soils and fluvial networks on land, and the freshwater content of the ocean. The changes in stores and fluxes of freshwater have a direct impact on biological systems, not only of the arctic region itself, but also well beyond its bounds. In this investigation, we used a heuristic, graphical approach to distill the system into its fundamental parts, documented the key relationships between those parts as best we know them, and identified the feedback loops within the system. The analysis illustrates relationships that are well understood, but also reveals others that are either unfamiliar, uncertain, or unexplored. The graphical approach was used to provide a visual assessment of the arctic hydrologic system in one possible future state in which the Arctic Ocean is seasonally ice free.