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