Citation Information

  • Title : Climate change impacts for the conterminous USA: an integrated assessment. Part 3. Dryland production of grain and forage crops.
  • Source : Climatic Change
  • Publisher : Springer Netherlands
  • Volume : 69
  • Issue : 1
  • Pages : 43-65
  • Year : 2005
  • DOI : 10.1007/1-4020-3
  • ISBN : 10.1007/1-4020-3876-3_4
  • Document Type : Journal Article
  • Language : English
  • Authors:
    • Rosenberg, N. J.
    • Brown, R. A.
    • Thomson, A. M.
    • Izaurralde, R. C.
    • Benson, V.
  • Climates:
  • Cropping Systems: Dryland cropping system. Maize. Legumes. Soybean. Wheat.
  • Countries: USA.

Summary

Here we simulate dryland agriculture in the United States in order to assess potential future agricultural production under a set of general circulation model (GCM)-based climate change scenarios. The total national production of three major grain crops - corn, soybeans, and winter wheat - and two forage crops - alfalfa and clover hay - is calculated for the actual present day core production area (CPA) of each of these crops. In general, higher global mean temperature (GMT) reduces production and higher atmospheric carbon dioxide concentration ([CO 2]) increases production. Depending on the climatic change scenarios employed overall national production of the crops studied changes by up to plus or minus 25% from present-day levels. Impacts are more significant regionally, with crop production varying by greater than 50% from baseline levels. Analysis of currently possible production areas (CPPAs) for each crop indicates that the regions most likely to be affected by climate change are those on the margins of the areas in which they are currently grown. Crop yield variability was found to be primarily influenced by local weather and geographic features rather than by large-scale changes in climate patterns and atmospheric composition. Future US agronomic potential will be significantly affected by the changes in climate projected here. The nature of the crop response will depend primarily on to what extent precipitation patterns change and also on the degree of warming experienced.

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