calcDODN | R Documentation |
The function estimates the DN value of a "dark object" which is used for atmospheric correction using the DOS2 and DOS4 model. Therefore, the frequency distribution of the smallest 1% of the data values is analyzed and the value for which the first derivate has the absolute maximum is taken as the DN for a dark object.
## S4 method for signature 'Satellite'
calcDODN(x, bcde)
## S4 method for signature 'RasterLayer'
calcDODN(x)
x |
Satellite object or RasterLayer with sensor band data, e.g. returned
by |
bcde |
If 'x' is a Satellite object, a band code as character. |
The DN for a dark object is extracted from a histogram similar to Chavez (1988).
Numeric value of the DN for the dark object.
Chavez Jr PS (1988) An improved dark-object subtraction technique for atmospheric scattering correction of multispectral data. Remote Sensing of Environment 24/3, \Sexpr[results=rd]{tools:::Rd_expr_doi("10.1016/0034-4257(88)90019-3")}.
The DN is used by calcPathRadDOS
for computing the
path radiance based on the dark object method.
path <- system.file("extdata", package = "satellite")
files <- list.files(path, pattern = glob2rx("LC08*.TIF"), full.names = TRUE)
sat <- satellite(files)
calcDODN(sat, bcde = "B002n")
calcDODN(getSatDataLayer(sat, bcde = "B002n"))
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