Options for Martian TimekeepingCopyright © 1997 by William Woodswwoods@ix.netcom.comIntroductionMars is unique in the Solar System. The natural conditions of the moons and asteroids are so harsh that humans will have to surround themselves with artificial environments. They will not need to change the systems of timekeeping we use on Earth. When they care about the position of the sun in the sky, they will find it out the same way that we find out the state of the tide: table look-up. By contrast, the environment of Mars is sufficiently hospitable that explorers and colonists will surely choose to adjust their lives to fit its pattern of days and seasons. This article examines the choices they (we!) can and should make. The primary, immovable constraints are set by nature: the length of the day, the length of the year, and the climatic cycle. The secondary constraints are set by human nature. In the first draft of this article, the phrase "for convenience, something should be thus-and-so" kept appearing. I've excised most of these; instead I'll say up front that this is an very important consideration. For instance, The day could be divided into 24 regular hours plus a short 25th hour, but this is needlessly inconvenient - therefore it's wrong. DaysStudies have shown that humans operate on a ~25 hour internal clock, which is reset every morning, so adjusting to Mars' 24 2/3 hour day will pose no problem. The SI second must remain the fundamental unit of time. Unfortunately, there is no reasonable way to use it as a subunit of the 88775.244 sec Martian day. For shift work, the Mday{1} must be divisible by 2, 3, and 4; hence by 12. Twenty-four Mhours would obviously work very well, but 60 might work even better. The Mhour need not be divided into 60x60 Msecs{2}. Instead we could decimalize, dividing the Mhour into 1000 or 100x100 Msomethings. SeasonsSince the Myear is so long, it could plausibly be divided into six or eight seasons. Or even into five, if the long slow trip past aphelion seemed to justify having two northern-summer seasons. Choosing the number of seasons restricts the choice for the calendar, since each season should be divided into the same number of whole months, and each year should be a set of whole seasons. The Martian year should be divided into seasons which divide the climatic cycle into coherent chunks, never mind the Martian Celestial Latitude of the sun. Getting this wrong forces people to talk about, for instance, the dust storms of the southern summer as happening in the late Spring & early Summer. The dust storm period should be inside one big season, or two small ones. On the other hand, there's no point in being too fussy, since the climatic cycle varies with location, especially with latitude. In parts of California, summer weather lasts more than half the year, while in Minnesota, "last year, summer fell on a Wednesday". On Earth, the old convention made summer and winter the quarters of the year with the most and least insolation. Summer ran from May Day through the solstice (Midsummer Day) to Lammas. Winter ran from Halloween to Groundhog Day. For some reason we shifted to the modern convention, in which these seasons run from solstice to equinox. Because of thermal inertia, the warmest and coldest quarters lag about a month behind the brightest and darkest quarters. On Mars, with a long year and no oceans (yet), the temperature must follow the insolation pretty closely. Except at the poles of course, where the seasonal dry-ice caps keep the temperature from falling below the sublimation point in the winter, and then keep it from rising well into the spring, after which it leaps up. Between the Tropics of Virgo and Pisces the variation of insolation is driven by the orbit's eccentricity, which takes Mars from 207 to 250 gigametres out from the sun. YearsA 668-day year can be divided 20 months of 33 or 34 days, grouped into four or five seasons. A 672-day year can be divided 24 four-week months (or 12 awfully long ones), grouped into 4, 6, or 8 seasons. The excess days can be subtracted from the last month of four seasons, or all from the last month of the year. With 668.592 days per year, the rule for intercalary days is pretty simple: years divisible by two and/or five have 669 days, years ending in 1, 3, 7, or 9 have 668 days (or alternately, years ending in 2, 4, 6, and 8 are short, the rest are long). For additional accuracy, centennial years are short, except for years divisible by 500. The 669th day should be added to the last month of long years. Month NamesThe Earth names for months could be adopted and extended: ... , November, December, Undecember, Duodecember, ... , perhaps as far as Quattourvigintember - but that would be awfully clunky. The names of months should be acceptable universally, preferably not even needing translation. For mnemonic convenience, they should be ordered in some way - alphabetical, numerical, chronological, ... Naming them for constellations would do nicely. Perizodiacal constellations can be used to pad the list of the canonical dozen. Year NumbersPutting the year 1 of the Martian Era in the recent past puts most of history on minus time. For convenient conversion, 0.0 ME should be close to AD 0.0 (actually, 1.0 BC). Then ME xxxx = AD yyyy/1.880868 + <a small constant>. However, the fiducial date should be modern. Mars had a southward (autumnal) equinox {3} at about AD 1975.1 ~= 1050.1 ME. This implies that the southward equinox should be in the first season of the Myear. This one could be defined as ME 10../dd, hh.mmss Airy Mean Time. Martian Celestial Longitude could be measured from the First Point of Taurus, a nice match for Earth's Aries. Options: Mday = 24 hours (3699 secs) = 24 x 60 minutes (61.65 secs) = 24 x 60 x 60 Somethings (1.0275 secs) = 24 x 60 x 100 Somethings (0.6165 secs) = 24 x 100 minutes (36.99 secs) = 24 x 100 x 100 Somethings ( 0.3699 secs) Mday = 60 1st units (24.67 Emins = 1480 secs) = 60 x 60 2nd units (24.66 secs) = 60 x 60 x 60 3rd units (0.4110 secs) = 60 x 100 2nd units (14.8 secs) = 60 x 100 x 10 3rd units (1.48 secs) = 60 x 100 x 100 3rd units (0.148 secs) Myear = 4 seasons (167 or 168 days) = 4 x 5 months (33 + 34 + 33 + 34 + [33 or 34] days) = 4 x 6 months (28 +..+ 28 + [27 or 28] days) = 5 seasons (133 or 134 days) = 5 x 4 months (33 + 34 + 33 + [33 or 34] days) = 6 seasons (111 or 112 days) = 6 x 4 months (28 + 28 + 28 + [27 or 28] days) = 8 seasons (83 or 84 days) = 8 x 3 months (28 + 28 + [27 or 28] days) Mars Data Mday = 1.02749125 Edays (Mday = Martian mean solar day) = 88775.244 SI sec = 24.659790 Ehours = 24h 39m 35.244s Myear = 686.9725 Edays (Myear = Martian tropical year) = 1.880868 Eyears = 7.5 Eseasons = 59354420. SI sec = 668.592 Mdays For example: Supposing a 24-month, four-season year, with solstices ~ in middle of 2nd and 4th seasons ( MDate 1050.151 = EDate 1975.124/Myear + 0.038 ). MDates are +/- a day or so, since an Mday overlaps 2 or 3 Edays.
EDate Event Lsun MDate -------------------------------------------------------------- Feb 16, 1975 Southward Equinox 180 1050/4/17 Aug 26, 1996 Northward Equinox 0 10../8 Jan 29, 1997 Aphelion 70 10../21 March 13, 1997 Northern Solstice 90 10../7 Sept 12, 1997 Southward Equinox 180 1062/4/18 Jan 7, 1998 Perihelion 250 1062/8/21 Feb 6, 1998 Southern Solstice 270 1062/9/22 July 14, 1998 Northward Equinox 0 10../9 Dec 17, 1998 Aphelion 70 10../22 Jan 29, 1999 Northern Solstice 90 10../8 Nov 7, 1996 Mars Global Surveyor Launch 10../23 Dec 4, 1996 Mars Pathfinder Launch 10../22 July 4, 1997 Mars Pathfinder Landing 1062../PRE>Sept 12, 1997 Mars Global Surveyor Capture 1062/4/18 |