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LSST Data Management Base Package
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Time scale to use when aligning TimeFrames. (string)
Valid values are listed in the Time Scales section (below).
This attribute controls how a TimeFrame behaves when it is used (by Frame::findFrame or Frame::convert) as a template to match another (target) TimeFrame. It identifies the time scale in which alignment is to occur. See the TimeScale attribute for a desription of the values which may be assigned to this attribute. The default AlignTimeScale value depends on the current value of TimeScale: if TimeScale is UT1, GMST, LMST or LAST, the default for AlignTimeScale is UT1, for all other TimeScales the default is TAI.
When Frame::findFrame or Frame::convert is used on two TimeFrames (potentially describing different time coordinate systems), it returns a Mapping which can be used to transform a position in one TimeFrame into the corresponding position in the other. The Mapping is made up of the following steps in the indicated order:
The offset from UTC to Local Time, in hours. (float)
This specifies the offset from UTC to Local Time, in hours (fractional hours can be supplied). It is positive for time zones east of Greenwich. AST uses the figure as given, without making any attempt to correct for daylight saving. The default value is zero.
The zero point for TimeFrame axis values. (float)
This specifies the origin from which all time values are measured. The default value (zero) results in the TimeFrame describing absolute time values in the system given by the System attribute (e.g. MJD, Julian epoch, etc). If a TimeFrame is to be used to describe elapsed time since some origin, the TimeOrigin attribute should be set to hold the required origin value. The TimeOrigin value stored inside the TimeFrame structure is modified whenever TimeFrame attribute values are changed so that it refers to the original moment in time.
The formats accepted when setting a TimeOrigin value are listed below. They are all case-insensitive and are generally tolerant of extra white space and alternative field delimiters:
When enquiring TimeOrigin values, the returned formatted floating point value represents a value in the TimeFrame's System, in the unit specified by the TimeFrame's Unit attribute.
Time scale. (string)
This attribute identifies the time scale to which the time axis values of a TimeFrame refer, and may take any of the values listed in the Time Scales section (below).
The default TimeScale value depends on the current System value; if the current TimeFrame system is "Besselian epoch" the default is "TT", otherwise it is "TAI". Note, if the System attribute is set so that the TimeFrame represents Besselian Epoch, then an error will be reported if an attempt is made to set the TimeScale to anything other than TT.
Note, the supported time scales fall into two groups. The first group containing UT1, GMST, LAST and LMST define time in terms of the orientation of the earth. The second group (containing all the remaining time scales) define time in terms of an atomic process. Since the rate of rotation of the earth varies in an unpredictable way, conversion between two timescales in different groups relies on a value being supplied for the Dut1 attribute (defined by the parent Frame class). This attribute specifies the difference between the UT1 and UTC time scales, in seconds, and defaults to zero. See the documentation for the Dut1 attribute for further details.
The TimeFrame class supports the following TimeScale values (all are case-insensitive):
An very informative description of these and other time scales is available at http://www.ucolick.org/~sla/leapsecs/timescales.html.
UTC should ideally be expressed using separate hours, minutes and seconds fields (or at least in seconds for a given date) if leap seconds are to be taken into account. Since the TimeFrame class represents each moment in time using a single floating point number (the axis value) there will be an ambiguity during a leap second. Thus an error of up to 1 second can result when using AST to convert a UTC time to another time scale if the time occurs within a leap second. Leap seconds occur at most twice a year, and are introduced to take account of variation in the rotation of the earth. The most recent leap second occurred on 1st January 1999. Although in the vast majority of cases leap second ambiguities won't matter, there are potential problems in on-line data acquisition systems and in critical applications involving taking the difference between two times.
1.9.5