A <- B <- B2 <- matrix( 0, 10, 12)
A[2,3] <- 3
B[4,7] <- 400
B2[10,12] <- 17
hold <- make.SpatialVx(A, list(B,B2), thresholds=c(0.1,3.1,500),
field.type="contrived", units="none",
data.name=c("Example", "A", "B", "B2"))
metrV(hold)
metrV(hold, model=c(1,2))
data(pert000)
data(pert001)
data(ICPg240Locs)
testobj <- make.SpatialVx(pert000, pert001, thresholds=1e-8,
projection=TRUE, map=TRUE, loc=ICPg240Locs, loc.byrow = TRUE,
field.type="Precipitation", units="mm/h",
data.name=c("ICP Perturbed Cases", "pert000", "pert001"))
metrV(testobj)
# compare above to results in Fig. 3 (top right panel) of Zhu et al. (2011).
data(geom000)
data(geom001)
testobj <- make.SpatialVx(geom000, geom001, thresholds=0,
projection=TRUE, map=TRUE, loc=ICPg240Locs, loc.byrow = TRUE,
field.type="Precipitation", units="mm/h",
data.name=c("ICP Geometric Cases", "geom000", "geom001"))
metrV(testobj)
# compare above to results in Fig. 2 (top right panel)
# of Zhu et al. (2011). Note that they differ wildly.
# Perhaps because an actual elliptical area is taken in
# the paper instead of finding the values from the fields
# themselves?
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