The [[
method works for all oce
objects, i.e.
objects inheriting from oce-class
. The purpose
is to insulate users from the internal details of oce
objects, by looking for items within the various storage
slots of the object. Items that are not actually stored in
the object can also be extracted, including derived data such
as potential temperature, the units of measurement for
the data, data-quality flags, etc.
# S4 method for ctd
[[(x, i, j, ...)
An ctd
object, i.e. one inheriting from ctd-class
.
Character string indicating the name of item to extract.
Optional additional information on the i
item.
Optional additional information (ignored).
If the specialized method produces no matches, the following generalized
method is applied. As with the specialized method, the procedure hinges
first on the values of i
and, optionally, j
. The work
proceeds in steps, by testing a sequence of possible conditions
in sequence.
A check is made as to whether i
names one of the standard
oce
slots. If so, [[
returns the slot contents of that slot.
Thus, x[["metadata"]]
will retrieve the metadata
slot,
while x[["data"]]
and x[["processingLog"]]
return
those slots.
If i
is a string ending in the
"Unit"
, then the characters preceding that string
are taken to be the name of an item in the data object, and a list
containing the unit is returned. This list consists of an item
named unit
, which is an expression
, and
an item named scale
, which is a string describing the
measurement scale. If the string ends in " unit"
, e.g.
x[["temperature unit"]]
(note the space),
then just the expression is returned, and if it ends in
" scale"
, then just the scale is returned.
If i
is a string ending in "Flag"
, then the corresponding
data-quality flag is returned (or NULL
if there is no such flag).
For example, x[["salinityFlag"]]
returns a vector of salinity
flags if x
is a ctd object.
If i
is "sigmaTheta"
, then the value of
swSigmaTheta(x)
is returned. Similarly,
"sigma0"
returns swSigma0(x)
and
"spice"
returns swSpice(x)
. Note that
these relate to seawater properties and only make sense for
certain object types.
After these possibilities are eliminated,
the action depends on whether j
has been provided.
If j
is not provided, or is the string ""
,
then i
is sought
in the metadata
slot, and then in the data
slot,
returning whichever is found first. In other words, if j
is not provided, the metadata
slot takes preference over
the data
slot. However, if j
is provided, then
it must be either the string "metadata"
or "data"
,
and it directs where to look.
If none of the above-listed conditions holds, then NULL
is returned,
without the issuance of a warning or error message. (This silent operation
is employed so that [[
will behave like the normal R version.)
Some uses of [[,ctd-method
involve direct retrieval of
items within the data
slot of the ctd
object,
while other uses involve calculations based on items in that
data
slot. For an example, all ctd
objects
should hold an item named temperature
in the data
slot, so for example x[["temperature"]]
will retrieve that
item. By contrast, x[["sigmaTheta"]]
is taken to be a
request to compute \(\sigma_\theta\), and so
it yields a call to swTheta(x)
even if
the data
slot of x
might happen to contain an item
named theta
. This can be confusing at first, but it tends
to lead to fewer surprises in everyday work, for otherwise the
user would be forced to check the contents of any ctd
object under analysis, to determine whether that item will be looked
up or computed. Nothing is lost in this scheme, since the data
within the object are always accessible with oceGetData
.
It should be noted that the accessor is set up to retrieve quantities
in conventional units. For example, read.ctd.sbe
is
used on a .cnv
file that stores pressure in psi, it will
be stored in the same unit within the ctd
object, but
x[["pressure"]]
will return a value that has been converted
to decibars. (To get pressure in PSI, use x[["pressurePSI"]]
.)
Similarly, temperature is
returned in the ITS-90 scale, with a conversion having been performed with
T90fromT68
, if the object holds temperature in
IPTS-68. Again, temperature on the IPTS-68
scale is returned with x@data$temperature
.
This preference for computed over stored quantities is accomplished
by first checking for computed quantities, and then falling
back to the general [[
method if no match is found.
Some quantities are optionally computed. For example, some data files
(e.g. the one upon which the section
dataset is based)
store nitrite
along with the sum of nitrite and nitrate, the
latter with name `NO2+NO3`
. In this case, e.g. x[["nitrate"]]
will detect the setup, and subtract nitrite from the sum to yield
nitrate.
The list given below provides notes on some quantities that are, or may be, computed.
conductivity
without a second argument (e.g. a[["conductivity"]]
)
returns the value stored in the object. However, if a second argument is given,
and it is string specifying a unit, then conversion is made to that unit. The
permitted units are: either ""
or "ratio"
(for ratio),
"uS/cm"
, "mS/cm"
and "S/m"
. The calculations are based on
the definition of conductivity ratio as the ratio between measured conductivity
and the standard value 4.2914 S/m.
CT
or Conservative Temperature
: Conservative Temperature,
computed with gsw_CT_from_t
in the gsw
package.
density
: seawater density, computed with swRho(x)
.
(Note that it may be better to call that function directly, to gain
control of the choice of equation of state, etc.)
depth
: Depth in metres below the surface, computed
with swDepth(x)
.
N2
: Square of Brunt-Vaisala frequency, computed with
swN2(x)
.
potential temperature
: Potential temperature in the
UNESCO formulation, computed with swTheta(x)
.
This is a synonym for theta
.
Rrho
: Density ratio, computed with swRrho(x)
.
SA
or Absolute Salinity
: Absolute Salinity,
computed with gsw_SA_from_SP
in the gsw
package.
The calculation involves location as well as measured water properties.
If the object x
does not containing information on the location,
then 30N and 60W is used for the calculation, and a warning is generated.
sigmaTheta
: A form of potential density anomaly, computed with
swSigmaTheta(x)
.
sigma0
Equal to sigmaTheta
, i.e. potential density anomaly
referenced to a pressure of 0dbar, computed with swSigma0(x)
.
sigma1
: Potential density anomaly
referenced to a pressure of 1000dbar, computed with swSigma1(x)
.
sigma2
: Potential density anomaly
referenced to a pressure of 2000dbar, computed with swSigma2(x)
.
sigma3
: Potential density anomaly
referenced to a pressure of 3000dbar, computed with swSigma3(x)
.
sigma4
: potential density anomaly
referenced to a pressure of 4000dbar, computed with swSigma4(x)
.
SP
: Salinity on the Practical Salinity Scale, which is
salinity
in the data
slot.
spice
or spiciness0
: a variable that is in some sense
orthogonal to density, calculated with swSpice(x)
.
Note that this is defined differently for eos="unesco"
and
eos="gsw"
.
SR
: Reference Salinity computed with
gsw_SR_from_SP
in the gsw
package.
Sstar
: Preformed Salinity computed with
gsw_SR_from_SP
in the gsw
package.
See SA
for a note on longitude and latitude.
theta
: potential temperature in the UNESCO formulation,
computed with swTheta(x)
. This is a synonym for
potential temperature
.
time
: returns either a vector of times, a single
time, or NULL
. A vector is returned if time
is present in the data
slot, or if a time can be
inferred from other entries in the data
slot (some of which,
such as the common timeS
, also employ
startTime
within the metadata
slot). A single
value is returned if the dataset only has information on the start
time (which is stored as startTime
within the metadata
slot. If it is impossible to determine the sampling time, then
NULL
is returned. These time variants occur, in the
present version of oce, only for data read by read.ctd.sbe
,
the documention of which explains how times are computed.
z
: Vertical coordinate in metres above the surface, computed with
swZ(x)
.
A two-step process is used to try to find the requested information. First, a class-specific function tries to find it, but if that fails, then a general function is used (see next section).
Other functions that extract parts of oce objects: [[,adp-method
,
[[,adv-method
,
[[,amsr-method
,
[[,argo-method
,
[[,bremen-method
,
[[,cm-method
,
[[,coastline-method
,
[[,echosounder-method
,
[[,g1sst-method
,
[[,gps-method
,
[[,ladp-method
,
[[,landsat-method
,
[[,lisst-method
,
[[,lobo-method
,
[[,met-method
, [[,oce-method
,
[[,odf-method
, [[,rsk-method
,
[[,sealevel-method
,
[[,section-method
,
[[,tidem-method
,
[[,topo-method
,
[[,windrose-method
,
[[<-,adv-method
Other things related to ctd data: [[<-,ctd-method
,
as.ctd
, cnvName2oceName
,
ctd-class
, ctdDecimate
,
ctdFindProfiles
, ctdRaw
,
ctdTrim
, ctd
,
handleFlags,ctd-method
,
initialize,ctd-method
,
initializeFlagScheme,ctd-method
,
oceNames2whpNames
,
oceUnits2whpUnits
,
plot,ctd-method
, plotProfile
,
plotScan
, plotTS
,
read.ctd.itp
, read.ctd.odf
,
read.ctd.sbe
,
read.ctd.woce.other
,
read.ctd.woce
, read.ctd
,
setFlags,ctd-method
,
subset,ctd-method
,
summary,ctd-method
,
woceNames2oceNames
,
woceUnit2oceUnit
, write.ctd
# NOT RUN {
data(ctd)
head(ctd[["temperature"]])
# }
Run the code above in your browser using DataLab