v.v.= β 0 + β 1 (temp) + β 2 (saln) + β 3 (temp*saln)

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V.v.= β 0 + β 1 (Temp) + β 2 (Saln) + β 3 (Temp*Saln). Urquhart et al. (2012) Remotely Sensed Estimates of Surface Salinity in the Chesapeake Bay: A Statistical Approach. RSE. 123. V. parahaemolyticus 9/18/2006. V. vulnificus 9/18/2006. - PowerPoint PPT Presentation

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Page 1: V.v.= β 0  + β 1 (Temp)  + β 2 (Saln)  + β 3 (Temp*Saln)
Page 2: V.v.= β 0  + β 1 (Temp)  + β 2 (Saln)  + β 3 (Temp*Saln)

V.v.= β0 + β1(Temp) + β2(Saln) + β3(Temp*Saln)

Urquhart et al. (2012) Remotely Sensed Estimates of Surface Salinity in the Chesapeake Bay: A Statistical Approach. RSE. 123

Page 3: V.v.= β 0  + β 1 (Temp)  + β 2 (Saln)  + β 3 (Temp*Saln)

Urquhart et al. (2013) Geospatial Interpolation of MODIS-derived Salinity and Temperature in the Chesapeake Bay. RSE. 135

V. vulnificus 9/18/2006 V. parahaemolyticus 9/18/2006