A Martian solar day is about 2.75% longer than Earth's solar day, having a mean (average) duration of 24 hours 39 minutes and 35.25 seconds. Planetary scientists consequently refer to a Martian solar day as a "sol" in order to avoid confusion between the two units of similar duration. The average length of Mars' tropical year, the interval between one occurrence of the vernal equinox and the next, is consequently 668.59 sols long, or 686.97 days in Earth units.
If the days on Mars have a different length than those on Earth, what about the hours, minutes and seconds? The 24-hour time readouts in Mars24 use Martian versions of these units -- i.e., Mars-hours, Mars-minutes, and Mars-seconds -- and which are about 2.75% longer than their Earth analogs. We choose this display method because of its familiarity; many if not most users would find a clock which ticks up to 24:39:35 before resetting to 00:00:00 quite confusing.
Why do we refer to "mean" time units? On all planets, values of the various orbital parameters combine such that the durations of days and sols are not constant throughout the year. On Earth, rather than reset our watches every day to read "12:00:00" at exactly high noon -- true solar noon -- we instead define 24 hours to be the mean duration of a solar day. As a result, the clock time at which the Sun is at its highest point varies a bit from day to day, going through an annual cycle of being anywhere from 14.2 minutes ahead of clock noon to 16.3 minutes behind it. Thus, the difference between mean and true solar time.
The discrepancy between clock noon and true solar noon for any day of the year may be calculated according to what is known as the Equation of Time, a graph of which reveals a shape called the analemma. This "figure eight" shape is often marked on Earth globes, usually in the empty space of the South Pacific, and on some sundials. A Mars analemma, however, is shaped more like a raindrop.
On Mars, the Equation of Time varies over a larger range than it does on Earth, from 51.1 minutes in advance of noon to 39.9 behind. Thus, over the course of a Martian year, the readings displayed by Mars24 for mean solar time and true solar time may differ by as much as those values.
People realized in the 19th century that if every town and city kept its own track of mean time then things like railroad schedules would be impossibly confusing. Consequently, time zones were created, and today all communities in a time zone use the mean time of the meridian at the center of the zone. Each time zone is approximately one hour wide, or 15°, excluding adjustments made for political boundaries and significant geographic features.
Mars24 may also display the local time at the selected location in terms of a local "Mars time zone". We have defined that Mars time zones are exactly 15° wide and are centered on 0°W, 15°W, 30°W, etc. (We have not attempted to provide names for these time zones, instead referring to "local mean zonal time" rather than, for example, "Olympus Standard Time".)
The prime meridian of Mars is defined by the location of the crater Airy-0, named in honor of the British astronomer who built the telescope at Greenwich whose location defines the prime meridian on Earth. Consequently the "standard" time for Mars may be referred to as "Airy Mean Time" (AMT) in analogy to Earth's Greenwich Mean Time (GMT). Because use of the term "GMT" has effectively been supplanted by Universal Coordinated Time, or UTC, we refer in Mars24 to a Mars analog called Mars Coordinated Time, or MTC, which is functionally equivalent to Airy Mean Time.
Although numerous calendar have been proposed for Mars, the current version of Mars24 uses none of them. We instead use the areocentric solar longitude, LS, to keep track of the seasons. This is a measurement of the angle that Mars has reached in its orbit since northern hemisphere vernal (spring) equinox, and so Ls values of 0°, 90°, 180°, and 270° respectively define the N.H. vernal equinox, summer solstice, autumnal equinox and winter solstice.
Discussion of the data and formulae used by Mars24 may be found in:
The time formulae were updated in January 2002 (i.e., for version 4.0 of Mars24) to include a revised specification of the location of the Mars prime meridian, replacing the equation provided in Table 4 of the Allison and McEwen paper. The new specification was reported in:
Additionally, the conversion between TT and UTC as given by Equation 27 of Allison and McEwen 2000 was modified by Dr. Allison in July 2003. In August 2003, the calculation of Mars' heliocentric longitude and latitude were refined, which in turn allowed for calculation of the light-distance between Earth and Mars to within one second.
Information about deriving mission time for the Mars Exploration Rovers was obtained from:
The current version of Mars24 may be found at http://www.giss.nasa.gov/tools/mars24/
Mars24 was written by Dr. Robert B. Schmunk. If you wish to be notified when new versions of Mars24 are released or if you would like to report a bug, please contact:
Robert B. Schmunk
NASA Goddard Institute for Space Studies
2880 Broadway
New York, NY 10025 USA
rschmunk@giss.nasa.gov