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B. I. Cook and R. Seager The response of the North American Monsoon to increased greenhouse gas forcing Journal of Geophysical Research: Atmospheres 118

Version of Record online: 27 FEB 2013 | DOI: 10.1002/jgrd.50111

Key Points

  • Warming suppresses early monsoon rainfall and enhances late monsoon rainfall
  • Early declines are caused by increased stability due to upper level warming
  • Later increases occur once moisture convergence can overcome increased stability

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