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Volume 23, Number 3—March 2017
Research

Spatiotemporal Fluctuations and Triggers of Ebola Virus Spillover

John Paul SchmidtComments to Author , Andrew W. Park, Andrew M. Kramer, Barbara A. Han, Laura W. Alexander, and John M. Drake
Author affiliations: University of Georgia Odum School of Ecology, Athens, Georgia, USA (J.P. Schmidt, A.W. Park, A.M. Kramer, J.M. Drake); University of Georgia Center for the Ecology of Infectious Diseases, Athens (J.P. Schmidt, A.W. Park, A.M. Kramer, J.M. Drake); Cary Institute of Ecosystem Studies, Millbrook, New York, USA (B.A. Han); University of California–Berkeley Department of Ecology, Berkeley, California, USA (L.W. Alexander)

Main Article

Figure 3

Phase graph showing the relationship between mean monthly rainfall and raw Ebola spillover intensity (defined as average density or expected number of points per unit area and/or time) for known Ebola virus disease locations in West and Central Africa (closed circles) and locations in northeastern or southern Africa where model results indicate moderate to high Ebola spillover intensity seasonally (open squares). Points are ordered by least to greatest monthly rainfall at each site. Dotted horiz

Figure 3. Phase graph showing the relationship between mean monthly rainfall and raw Ebola spillover intensity (defined as average density or expected number of points per unit area and/or time) for known Ebola virus disease locations in West and Central Africa (closed circles) and locations in northeastern or southern Africa where model results indicate moderate to high Ebola spillover intensity seasonally (open squares). Points are ordered by least to greatest monthly rainfall at each site. DRC, Democratic Republic of the Congo.

Main Article

Page created: February 24, 2017
Page updated: February 24, 2017
Page reviewed: February 24, 2017
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