Hello everyone,
Quite a long time ago (it was in 2011, when I checked back!) Trekguide.com raised the question of whether it was possible to work out how long a Vulcan year might be, using the available evidence. At the time, I thought I was a few tweaks away from having a finished timeline that would address this very question, and some preliminary ideas about Vulcan itself. I’ve reused the original thread title (and made it a sequel), rather than trying to resuscitate it after all this time. A lot of the ideas raised in that thread have been enormously helpful, and I’ve changed my mind about quite a lot of what I said four years ago, now that I’ve looked at things in more detail.
As it turned out, the few tweaks I had in mind for my timeline turned into a lot of reworking. The end result isn’t very different from what I had before, but it all had to be carefully revisited. There’s a link to it at the bottom of this message, but looking at the website is an “optional extra,” not what this (long) post is about.
I have to stress that although I think it is impossible to work out just one aspect of “Star Trek” chronology in isolation, there are no right answers. At every step, there are decisions to be made. My end result is one option, and there are a lot of alternatives. My particular calculations made it very plain six “Vulcan years” would be very, very close in length to seven Earth years. It might seem coincidental, but it would explain why such notoriously accurate people as Vulcans are content to settle with “seven years” as the average length of time between pon farr, rather than specifying 6.9 or 7.3 Earth years, for example.
So that’s what I’ve gone with. It means that Tuvok hasn’t yet celebrated his 100th Vulcan years birthday in “Fury.” I’ve compiled more detail about the life events of Spock, Tuvok and T’Pol here:
http://atavachron.wikidot.com/calendars:my-vulcan-calendar
The big question is whether I can then construct a “planet Vulcan” that isn’t immediately scientifically impossible, but fits in with as much of the information we have as I can make it. Firstly, I’ve had to assume that my “Vulcan year” isn’t a single orbit of Vulcan around its star. Since I want to put Vulcan in the 40 Eridani star system, there was no plausible way a hot desert planet could have an orbit that lasted so long. The planet would be too far from the star, especially since it has a thin atmosphere, making elaborate “greenhouse” explanations of a high surface temperature unlikely. Instead, I’ve adopted the idea that the Vulcan time unit equivalent to a “year” lasts two orbits. This puts my hypothetical Vulcan much closer in. At that distance, the level of light from the star is a little above the amount Earth gets from the Sun. Not too much to rule out an inhabited planet, but certainly in line with the suggestion of more intense sunlight on Vulcan. (Remember Mister Spock’s extra eyelid?)
I then needed to look at the question of what the view from the surface of Vulcan might look like, based on the Vulcan day being around the same as an Earth day (no mention is ever made of it being remarkably long or short, and the days and nights in stories set on Vulcan seem to match quite closely with a conventional day). I adopted a “Vulcan day” from Geoffrey Mandel’s “U.S.S. Enterprise Officer’s Manual” of 1.113 Earth days, rather than making something up at random.
In the original thread, T’Girl suggested that the clearest evidence for a “sister planet” is the “ice world” in the 2009 “Star Trek” film. After looking at all the evidence, I can only agree, although I didn’t at the time of the original thread. But is it possible for a desert world and an ice planet to share an orbit? To my considerable surprise, I think it is. Once you assume that red planet Vulcan absorbs a lot of the light and heat reaching it from 40 Eridani A, and that the pale ice world is much, much more reflective, then there’s a huge temperature difference. By using the albedo figures for Mars and Venus (although the surface of Venus is very hot, the top of the Venusian clouds are pale, and reflect a lot of light, easily as much as an ice planet might) I calculated that what you might call the “base” or more properly the “blackbody” temperature of my version of Vulcan would come out about 4 degrees Celsius (7 degrees Fahrenheit) warmer than Earth. The ice world would be about 95 degrees Celsius (171 degrees Fahrenheit) colder than Earth. Even taking into account the insulating and warming effects of the atmospheres of the planets, there can be a huge difference in average temperature between the two, enough for one to be desert and the other covered completely in ice. My calculations are here:
http://atavachron.wikidot.com/calendars:building-vulcan
I’ve also tried to fill in some plausible numbers for things like gravity for the two worlds, and cobbled together some rough visualisations of what my version of things ought to look like, here:
http://atavachron.wikidot.com/calendars:putting-it-together
(I’m afraid I can’t show the images direct; not enough posts.)
The only thing I’m dubious about is the “little moon” seen in “Star Trek: The Motion Picture.” In order to stay in orbit around the ice planet, it needs to be very, very close in. Although it’s more of a guess than anything else, I’m not sure that there’s enough room for even a tiny moon to stay in place, without either being caught by the ice planet’s atmosphere with catastrophic results, or being pulled into an unstable orbit by Vulcan, again with usually catastrophic results. In the end, I’ve sort of assumed that it’ll work, because we see it. It’s the bit of the whole set-up I’m least happy with, though.
Thanks for reading through this enormous post. Unfortunately, I can’t say I’ve found any final answers, because there are just too many variables. It was fun trying to “build a planet,” and I hope that it all doesn’t fall apart once someone who understands the science and maths takes a look at it.
I actually had all this stuff ready to go last month, but it really didn’t feel like the right time.
Best wishes,
Timon
Quite a long time ago (it was in 2011, when I checked back!) Trekguide.com raised the question of whether it was possible to work out how long a Vulcan year might be, using the available evidence. At the time, I thought I was a few tweaks away from having a finished timeline that would address this very question, and some preliminary ideas about Vulcan itself. I’ve reused the original thread title (and made it a sequel), rather than trying to resuscitate it after all this time. A lot of the ideas raised in that thread have been enormously helpful, and I’ve changed my mind about quite a lot of what I said four years ago, now that I’ve looked at things in more detail.
As it turned out, the few tweaks I had in mind for my timeline turned into a lot of reworking. The end result isn’t very different from what I had before, but it all had to be carefully revisited. There’s a link to it at the bottom of this message, but looking at the website is an “optional extra,” not what this (long) post is about.
I have to stress that although I think it is impossible to work out just one aspect of “Star Trek” chronology in isolation, there are no right answers. At every step, there are decisions to be made. My end result is one option, and there are a lot of alternatives. My particular calculations made it very plain six “Vulcan years” would be very, very close in length to seven Earth years. It might seem coincidental, but it would explain why such notoriously accurate people as Vulcans are content to settle with “seven years” as the average length of time between pon farr, rather than specifying 6.9 or 7.3 Earth years, for example.
So that’s what I’ve gone with. It means that Tuvok hasn’t yet celebrated his 100th Vulcan years birthday in “Fury.” I’ve compiled more detail about the life events of Spock, Tuvok and T’Pol here:
http://atavachron.wikidot.com/calendars:my-vulcan-calendar
The big question is whether I can then construct a “planet Vulcan” that isn’t immediately scientifically impossible, but fits in with as much of the information we have as I can make it. Firstly, I’ve had to assume that my “Vulcan year” isn’t a single orbit of Vulcan around its star. Since I want to put Vulcan in the 40 Eridani star system, there was no plausible way a hot desert planet could have an orbit that lasted so long. The planet would be too far from the star, especially since it has a thin atmosphere, making elaborate “greenhouse” explanations of a high surface temperature unlikely. Instead, I’ve adopted the idea that the Vulcan time unit equivalent to a “year” lasts two orbits. This puts my hypothetical Vulcan much closer in. At that distance, the level of light from the star is a little above the amount Earth gets from the Sun. Not too much to rule out an inhabited planet, but certainly in line with the suggestion of more intense sunlight on Vulcan. (Remember Mister Spock’s extra eyelid?)
I then needed to look at the question of what the view from the surface of Vulcan might look like, based on the Vulcan day being around the same as an Earth day (no mention is ever made of it being remarkably long or short, and the days and nights in stories set on Vulcan seem to match quite closely with a conventional day). I adopted a “Vulcan day” from Geoffrey Mandel’s “U.S.S. Enterprise Officer’s Manual” of 1.113 Earth days, rather than making something up at random.
In the original thread, T’Girl suggested that the clearest evidence for a “sister planet” is the “ice world” in the 2009 “Star Trek” film. After looking at all the evidence, I can only agree, although I didn’t at the time of the original thread. But is it possible for a desert world and an ice planet to share an orbit? To my considerable surprise, I think it is. Once you assume that red planet Vulcan absorbs a lot of the light and heat reaching it from 40 Eridani A, and that the pale ice world is much, much more reflective, then there’s a huge temperature difference. By using the albedo figures for Mars and Venus (although the surface of Venus is very hot, the top of the Venusian clouds are pale, and reflect a lot of light, easily as much as an ice planet might) I calculated that what you might call the “base” or more properly the “blackbody” temperature of my version of Vulcan would come out about 4 degrees Celsius (7 degrees Fahrenheit) warmer than Earth. The ice world would be about 95 degrees Celsius (171 degrees Fahrenheit) colder than Earth. Even taking into account the insulating and warming effects of the atmospheres of the planets, there can be a huge difference in average temperature between the two, enough for one to be desert and the other covered completely in ice. My calculations are here:
http://atavachron.wikidot.com/calendars:building-vulcan
I’ve also tried to fill in some plausible numbers for things like gravity for the two worlds, and cobbled together some rough visualisations of what my version of things ought to look like, here:
http://atavachron.wikidot.com/calendars:putting-it-together
(I’m afraid I can’t show the images direct; not enough posts.)
The only thing I’m dubious about is the “little moon” seen in “Star Trek: The Motion Picture.” In order to stay in orbit around the ice planet, it needs to be very, very close in. Although it’s more of a guess than anything else, I’m not sure that there’s enough room for even a tiny moon to stay in place, without either being caught by the ice planet’s atmosphere with catastrophic results, or being pulled into an unstable orbit by Vulcan, again with usually catastrophic results. In the end, I’ve sort of assumed that it’ll work, because we see it. It’s the bit of the whole set-up I’m least happy with, though.
Thanks for reading through this enormous post. Unfortunately, I can’t say I’ve found any final answers, because there are just too many variables. It was fun trying to “build a planet,” and I hope that it all doesn’t fall apart once someone who understands the science and maths takes a look at it.
I actually had all this stuff ready to go last month, but it really didn’t feel like the right time.
Best wishes,
Timon