Vulnerability of Northern Prairie Wetlands to Climate Change

Abstract The prairie pothole region (PPR) lies in the heart of North America and contains millions of glacially formed, depressional wetlands embedded in a landscape matrix of natural grassland and agriculture. These wetlands provide valuable ecosystem services and produce 50% to 80% of the continent's ducks. We explored the broad spatial and temporal patterns across the PPR between climate and wetland water levels and vegetation by applying a wetland simulation model (WETSIM) to 18 stations with 95-year weather records. Simulations suggest that the most productive habitat for breeding waterfowl would shift under a drier climate from the center of the PPR (the Dakotas and southeastern Saskatchewan) to the wetter eastern and northern fringes, areas currently less productive or where most wetlands have been drained. Unless these wetlands are protected and restored, there is little insurance for waterfowl against future climate warming. WETSIM can assist wetland managers in allocating restoration dollars in an uncertain climate future.

[1]  I. J. Ball,et al.  Sensitivity analyses of the life cycle of midcontinent mallards , 2002 .

[2]  M. W. Weller,et al.  Role of habitat in the distribution and abundance of marsh birds , 1965 .

[3]  M. Noguer,et al.  Climate change 2001: The scientific basis. Contribution of Working Group I to the Third Assessment Report of the Intergovernmental Panel on Climate Change , 2002 .

[4]  K. A. Poiani,et al.  Global warming and prairie wetlands , 1991 .

[5]  J. E. Weaver,et al.  History of the Native Vegetation of Western Kansas during Seven Years of Continuous Drought , 1942 .

[6]  A. V. D. Valk,et al.  Northern Prairie Wetlands , 1988 .

[7]  J. Houghton,et al.  Climate change 2001 : the scientific basis , 2001 .

[8]  James M. Omernik,et al.  Ecoregions: A Spatial Framework for Environmental Management , 1995 .

[9]  Thomas C. Winter,et al.  Hydrology of Prairie Pothole Wetlands during Drought and Deluge: A 17-Year Study of the Cottonwood Lake Wetland Complex in North Dakota in the Perspective of Longer Term Measured and Proxy Hydrological Records , 1998 .

[10]  T. C. Winter,et al.  Climate change and northern prairie wetlands: Simulations of long-term dynamics , 1995 .

[11]  W. R. Osterkamp,et al.  Late-Holocene flooding and drought in the Northern Great Plains, USA, reconstructed from tree rings, lake sediments and ancient shorelines , 2005 .

[12]  J. Overpeck,et al.  2000 Years of Drought Variability in the Central United States , 1998 .

[13]  T. C. Winter Hydrological, chemical, and biological characteristics of a prairie pothole wetland complex under highly variable climate conditions : the Cottonwood Lake area, east-central North Dakota , 2003 .

[14]  D. Larson Effects of climate on numbers of northern prairie wetlands , 1995 .

[15]  C. B. Davis,et al.  The Role of Seed Banks in the Vegetation Dynamics of Prairie Glacial Marshes , 1978 .

[16]  J. Austin Responses of Dabbling Ducks to Wetland Conditions in the Prairie Pothole Region , 2002 .

[17]  Michael G. Anderson,et al.  Potential Effects of Global Warming on Waterfowl Populations Breeding in the Northern Great Plains , 1998 .

[18]  Wayne S. Davis,et al.  Biological assessment and criteria : tools for water resource planning and decision making , 1995 .

[19]  John R. Williams,et al.  EPIC-erosion/productivity impact calculator: 1. Model documentation. , 1990 .

[20]  John R. Williams,et al.  EPIC-erosion/productivity impact calculator: 2. User manual. , 1990 .

[21]  Md. Salequzzaman,et al.  Ecoregions: A Spatial Framework for Environmental Management , 2005 .

[22]  Stephen P. Brooks,et al.  Density dependence in North American ducks , 2004 .

[23]  Andrew N. Sharpley,et al.  EPIC, Erosion/Productivity Impact Calculator , 1990 .

[24]  Thomas C. Winter,et al.  THE VULNERABILITY OF WETLANDS TO CLIMATE CHANGE: A HYDROLOGIC LANDSCAPE PERSPECTIVE 1 , 2000 .

[25]  George H. Hargreaves,et al.  Defining and Using Reference Evapotranspiration , 1994 .