deltamm(object, x, y = NULL, max.delta = Inf, time.point = 1,
model = 1, verbose = FALSE, ...)## S3 method for class 'matched':
plot(x, ..., set.pw = FALSE,
horizontal = TRUE, loc.byrow = TRUE)
centmatch(object, x, y = NULL, criteria = 1, const = 14, time.point = 1,
model = 1, verbose = FALSE)
FeatureSutie
function, but does utilize information from its attributes. Can be missing.deltamm
, a list object with components X.feats
and Y.feats
, each of which are list objects containing numbered components within which are objects of class criteria
is 3.image.plot
from deltamm
: additional optional arguments to the deltametric
function from package plot.matched
, additional arguments to the plot
function. May use no.label
(logideltamm
:Gilleland et al. (2008) describe a method for automatically merging, and simultaneously, matching identified objects within two fields (a verification set). The method was proposed with the general method for spatial forecast verification introduced by Davis et al. (2006 a,b) in mind. It relies heavily on use of a binary image metric introduced by Baddeley (1992a,b) for comparing binary images; henceforth referred to as the delta metric, or just delta.
The procedure is as follows. Suppose there are m identified forecast features and n identified verification features.
1. Compute delta for each feature identified in the forecast field against each feature identified in the verification field. Store these values in an m by n matrix, Upsilon.
2. For each of the m rows of Upsilon, rank the values of delta to identify the features, j_1, ..., j_n that provide the lowest (best) to highest (worst) value, and do the same for each of the n columns to find the forecast features i1, ...,i_m that yield the lowest to highest values for each verification feature.
3. Create a new m by n matrix, Psi, whose columns contain delta computed between each of the individual features in the forecast and (first column) the corresponding j_1 feature from the verification field, and each successive column, k, has delta between the i-th forecast feature and the union of j_1, j_2, ..., j_k.
4. Create a similar m by n matrix, Ksi, that has delta computed between each individual feature in the verification field and the successively bigger unions i_1, ..., i_l for the l-th column.
5. Let Q=[Upsilon, Psi, Ksi], and merge and match objects based on the rankings of delta in Q. That is, find the smallest delta in Q, and determine which mergings (if any) and matchings correspond to this value. Remove the appropriate row(s) and column(s) of Q corresponding to the already determined matchings and/or mergings. Repeat this until all features in at least one field have been exhausted.
The above algorithm suffers from two deficiencies. First, features that are merged in one field cannot be matched to merged features in another field. One possible remedy for this is to run this algorithm twice, though this is not a universally good solution. Second, features can be merged and/or matched to features that are very different from each other. A possible remedy for this is to use the cut-off argument, max.delta, to disallow mergings or matchings between features whose delta value is not <= this="" cut-off.="" in="" practice,="" these="" two="" deficiencies="" are="" not="" likely="" very="" problematic.<="" p="">
centmatch
:
This function works similarly as deltamm
in that it is designed to work with FeatureSuite
with the same end of matching (but not merging) objects between fields. It is based on the method proposed by Davis et al. (2006a).
Baddeley, A. (1992b) Errors in binary images and an Lp version of the Hausdorff metric. Nieuw Arch. Wiskunde, 10, 157--183.
Davis, C. A., Brown, B. G. and Bullock, R. G. (2006a) Object-based verification of precipitation forecasts, Part I: Methodology and application to mesoscale rain areas. Mon. Wea. Rev., 134, 1772--1784.
Davis, C. A., Brown, B. G. and Bullock, R. G. (2006b) Object-based verification of precipitation forecasts, Part II: Application to convective rain systems. Mon. Wea. Rev., 134, 1785--1795.
Gilleland, E., Lee, T. C. M., Halley Gotway, J., Bullock, R. G. and Brown, B. G. (2008) Computationally efficient spatial forecast verification using Baddeley's delta image metric. Mon. Wea. Rev., 136, 1747--1757.
convthresh
, disjointer
, deltametric
, FeatureSuite
, owin
, tess
, tiles
, connected
x <- y <- matrix(0, 100, 100)
x[2:3,c(3:6, 8:10)] <- 1
y[c(4:7, 9:10),c(7:9, 11:12)] <- 1
x[30:50,45:65] <- 1
y[c(22:24, 99:100),c(50:52, 99:100)] <- 1
hold <- make.SpatialVx(x, y, field.type="contrived", units="none",
data.name=c("Example", "x", "y"))
look <- convthresh(hold, smoothpar=0.5)
par( mfrow=c(1,2))
image.plot(look$X.labeled)
image.plot(look$Y.labeled)
look2 <- deltamm(hold, x=look)
look3 <- centmatch(hold, x=look)
data(pert000)
data(pert004)
data(ICPg240Locs)
hold <- make.SpatialVx(pert000, pert004,
loc=ICPg240Locs, projection=TRUE, map=TRUE,
field.type="Precipitation", units="mm/h",
data.name=c("ICP Perturbed Cases", "pert000", "pert004"))
look <- convthresh(hold, smoothpar=10.5)
plot(look, set.pw=TRUE)
look2 <- deltamm(hold, x=look, verbose=TRUE)
plot(look2, set.pw=TRUE)
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