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Has Titan’s atmosphere expanded? Check out this article;
http://www.nasa.gov/missions/solarsyste … ncrab.html
Note this part;
Images showed that the diameter of Titan's X-ray shadow was larger than the diameter of the moon's solid surface. Why the difference? The answer: Titan's atmosphere. The difference in diameters reveals that the X-ray absorbing region of the moon's atmosphere reaches from the surface to a height of about 550 miles.
The upper atmosphere's extent is consistent with Voyager 1's 1980 measurements, or 10-15 percent larger. But according to Hiroshi Tsunemi of Japan's Osaka University, Saturn was closer to the sun in 2003, so possibly prompting Titan's atmosphere to expand slightly from increased solar heating.
Possibly here;
http://www.msss.com/moc_gallery/ab1_m04 … 304128.jpg
Notice the channels running from several craters.
Could the impactors that formed these crater punched down to the water table (If one exists) To the south the land rises considerably. To get an artesian well, part of the water table needs to be higher than the exit point. If there was a water table starting in the higher southern region, it would run downhill, and then it would surface where ever an impactor punched down to it.
Talk about life causing the dark bands that only show up in UV light has been around for a while. I forget which probe discover it. I have seen it mentioned in a couple of science fiction books. I didn’t know it was still being discussed last year. I guess they still have not found a satisfactory non-biological explanation.
If there microbes in the upper atmosphere, how did they get there. Did Venus once have a watery past? I read an Astronomy Article years ago that said Venus briefly had oceans of water way back in its past. Could they have evolved back then and survived all these years?
Could they have come from rocks blasted off the Earth by imp actors? Such meteors might burst in Venus’ upper atmosphere, scattering any bacteria that was in it. Could bacteria survive such a journey?
That was it- Shoemaker-Levy. Has it been 10 years? Wow! Time flies. I saw the dark spots on Jupiter with my little scope.
If it had hit Mars, I think it would have increased the air pressure. It would have also caused some localized floods. I don’t know how long the water would have stayed liquid, but it would have been great to study it.
Could it have caused rain for a short time around the point of impact?
Frost is possible, but I don't think it would last long during the day. It tends to quickly evaporate in the dry air. It could always form again the next night.
One of the Vikings observed frost on the surface.
Doh! I hate it when I make grammar errors. That should be
"I do disagree with the Author about Alpha Centauri C and Red Giants. We shouldn’t write them off yet. They may surprise us, just like Europa’s possible ocean surprised us."
I read this article in Astronomy Magazine many years ago. I am glad to see it on the internet. It is one of my favorite Astronomy articles.
[http://homepage.sunrise.ch/homepage/sch … tauri.html]http://homepage.sunrise.ch/homepage/sch … tauri.html
There could be up to 4 (Unlikely but possible) habitable planets in the Alpha Centauri system. If you placed the Solar System around Alpha Centauri A, Earth and Mars would be in the Life-zone. If you placed our Solar System Around Alpha Centauri B, Venus and Earth would be in the Life-zone.
I do disagree with the Author about Alpha Centauri C and Red Giants. Would shouldn’t write them off yet. They may surprise us, just like Europa’s possible ocean surprised us.
Humans should terraform Mars. We should spread life to dead worlds.
Mars should be studied first, and then terraformed.
If there are native microbes, that are not related to Earth microbes (There is a chance impactors could have send microbes from Earth to Mars and Mars to Earth), they should be studies and preserved in some Microbe Mars Zoo, before Mars is terraformed. If there are any Martian Microbes, they have not evolved much and are unlikely to before the Sun dies in 4 million years. They should not hamper human terraformation of Mars.
Many of our landers are located in areas that would be flooded by terraforming. I am sure they will be moved and put in Mars museums before terraformation.
As humans spread out into the galaxy, we will rarly find Class M (Teasing Star Trek) worlds we can live on with no terraforming. Most world will need some kind of terraforming. What we learn terraforming Mars and Venus will help us terraform worlds we find around other stars.
Antarctica and India meteorites linked to the same origins as Bounce. Bounce came from elsewhere on Mars than the region around Eagle Crater.
Check out the end of this press release;
[http://marsrovers.jpl.nasa.gov/gallery/ … 0414a.html]http://marsrovers.jpl.nasa.gov/gallery....4a.html
'Bounce' and Shergotty Share Common Ground
This illustration compares the light signature or spectrum of "Bounce," a rock at Meridiani Planum, to that of a martian meteorite found on Earth called Shergotty. Bounce's spectrum, and thus mineral composition, is unique to the rocks studies so far at Merdiani Planum and Gusev Crater, the landings sites of the Mars Exploration Rovers Opportunity and Spirit. However, the results here indicate that Bounce is not a one-of-a-kind rock, but shares origins with Shergotty. Shergotty landed in India in 1865. Bounce's spectra were taken on sol 67 by Opportunity's Moessbauer spectrometer.
And
Meteorite Linked to Rock at Meridiani
This meteorite, a basalt lava rock nearly indistinguishable from many Earth rocks, provided the first strong proof that meteorites could come from Mars. Originally weighing nearly 8 kilograms (17.6 pounds), it was collected in 1979 in the Elephant Moraine area of Antarctica. The side of the cube at the lower left in this image measures 1 centimeter (0.4 inches).
This picture shows a sawn face of this fine-grained gray rock. (The vertical stripes are saw marks.) The black patches in the rock are melted rock, or glass, formed when a large meteorite hit Mars near the rock. The meteorite impact probably threw this rock, dubbed "EETA79001," off Mars and toward Antarctica on Earth. The black glass contains traces of martian atmosphere gases.
The Mars Exploration Rover Opportunity has discovered that a rock dubbed "Bounce" at Meridiani Planum has a very similar mineral composition to this meteorite and likely shares common origins. Bounce itself is thought to have originated outside the area surrounding Opportunity's landing site; an impact or collision likely threw the rock away from its primary home.
Hi Shaun
The whole northern Nilosyrtis Mensae does scream ice. It looks like glacier activity went on in the past and may still be going on today. It certainly looks like active glaciers to me.
Those channels in the southern Nilosyrtis Mensae region puzzle me. I have search for other explanations but I keep coming back to water channels.
1. They all seem to originate from impact craters, one per crater.
2. They are all very long, suggesting that something very fluid created them.
The only thing I can think if is underground water. I don’t think they have water flowing in them at this moment (I would suspect if this was the case, they would have an ice coating covering them), but it looks like it was very recent.
I am an amateur Geologist and have even taught Geology at the High School and Jr. High level, but I have found that all my Geology experience doesn’t always help me with Mars. Mars is its own planet separate from Earth. It does have characteristics of the Earth, but it also has characteristics of the Moon. Mars is a cross between the Earth and the Moon in size and environment. (It does get less solar radiation than the Earth/Moon system) Mars is…well, Mars is its own planet with its own characteristics.
I have read more than one science article (I think one was in Discover Magazine) that the Earth looses water in space because the sunlight will break down water into oxygen and hydrogen. However the rate loss is compensated by comets so that there is no net loss.
Considering this, and the possibility comets may have deposited water ice at the Moons poles, and Mercury’s poles, then Mars probably get replenished with water from comets.
Too bad that comet that hit Jupiter a few years ago didn’t hit Mars.
Bounce, a rock that Opportunity studied, was shown to be Basalt, which is different from those rocks in Eagle crater. I was initially surprised at these findings, since it looked like the rocks in Eagle crater.
It seems to me that the light native rock of this area of Mars weathers quickly, leaving behind the harder, darker, blueberries. I guess I should have not been surprised that bounce was not from this area, seeing that it has not weathered as quickly as the native rock.
Opportunity is now at a crater called Fram
See:
[http://marsrovers.jpl.nasa.gov/gallery/ … _n084.html]http://marsrovers.jpl.nasa.gov/gallery/ … _n084.html
Fram looks like it could be younger than Eagle crater. Its rocks do not appear to be nearly as eroded.
bolbuyk, I don't know what a safe range would be for asteroids. It would need to be in a stable cycle, and there would need to be all kinds of fail-safe plans in case it was ever a threat to Earth, Mars or the Moon.
The pressure and temperature sometimes reaches the point to where liquid water can exist at the surface deep in the Hellas Basin. In Mars dry air, it would quickly evaporate, but it could exist just cm’s underground.
Here is a question I have wondered for a long time. Are their underground steams (Rivers) on Mars. Could pressure build enough in underground caverns long enough for water to stay stable as a liquid?
I have searched for in MOC pictures for springs that would confirm underground water. The closest I have found is in the Nilosyrtis Mensae region (See my thread on that)
Earthfirst, Flooding parts of the Sahara with the Mediterranean is not a bad idea. It might help lower the total seal level some.
I have thought about pumping seawater into central Antarctica to lower the sea level. Doing so would help increase the total land area of the Earth. For example, here in Texas, during the last couple of Ice Ages, the coast was over 100 miles downriver from where it is today.
Kippy, I have not done the math (Not sure if I even know the calculations ) but my gut feeling is that if Venus sunlight was cut 100% it wouldn't take long, maybe a year or two. The darkness of space is cold.
I guess the whole list was too big to post. You can see an example, anyway.
The list coveres the Alpha Centauri Systems (All three stars)
The Solar System looks like this;
I. The Solar System US/2295 8,331,116,750
A.*Earth UNSA/2054 7,347,790,120 7,347,790,120
B. Mars UNSA/2177 98,281,290 98,366,210
1. Phobos Mars/2231 73,540
2. Deimos Mars/2271 11,380
C. Mercury UNSA/2248 2,322,760 2,322,760
D. Ganymede UNSA/2248 5,726,020 9,510,480
1. Callisto Gany/2251 2,906,910
2. Europa Gany/2253 824,210
3. Io Gany/2253 16,290
4. Thebe Gany/2261 23,270
5. Himalia Gany/2264 4,620
6. Lysithea Gany/2265 1,530
7. Elara Gany/2279 6,940
8. Leda Gany/2291 690
E. Ceres UNSA/2253 272,510 469,170
1. Vesta Cere/2262 40,030
2. Pallas Cere/2262 12,180
3. Hygia Cere/2266 19,620
4. Davida Cere/2271 2,570
5. Interamnia Cere/2271 79,720
6. Eunomia Cere/2271 7,140
7. Sylvia Cere/2271 1,820
8. Cybele Cere/2271 730
9. Juno Cere/2277 23,780
10. Bamberga Cere/2277 1,040
11. Herculina Cere/2278 3,340
12. Patientia Cere/2283 800
13. Thalia Cere/2289 260
14. Mathilde Cere/2295 3,630
F. Venus UNSA/2270 52,639,280 52,639,280
G. Moon UNSA/2271 811,839,880 811,839,880
H. Titan UNSA/2274 8,040,820 8,091,070
1. Rhea Tita/2274 15,370
2. Iapetus Tita/2275 3,000
3. Dione Tita/2278 9,300
4. Tethys Tita/2281 2,790
5. Enceladus Tita/2286 11,040
6. Mimas Tita/2287 6,270
7. Hyperion Tita/2291 380
8. Janus Tita/2295 1,410
9. Pandora Tita/2295 690
I. Triton UNSA/2284 33,410 40,950
1. Pluto Trit/2285 4,570
2. Chiron Trit/2285 1,040
3. Nereid Trit/2287 920
4. Proteus Trit/2290 730
5. Thalassa Trit/2293 280
J. Miranda UNSA/2288 16,830 46,830
1. Oberon Mira/2288 7,660
2. Umbriel Mira/2288 3,570
3. Ariel Mira/2289 2,190
4. Titania Mira/2290 14,920
5. Cordelia Mira/2290 620
6. Portia Mira/2293 190
7. Cressida Mira/2294 850
In my story, "War Against Gravity" (I wrote it several years ago, when I was a bit younger) I set up the government like this. I thought this might be a way to set up a new multi-planet government.
Appendix 6
The Government Structure*
*As of the year 2295
The United Systems
Founded: March 15, 2295.
Capital Location: Earth’s Moon
Population:8,332,563,470
Each world, or nation, under the United Systems is independent. All systems disputes are settled through the United Systems. All Individual System Member(ISM) world disputes are settled through the individual systems central government. All World disputes are settled through the INS.
Chain of government:
United Systems
|
Star Systems
|
ISM World
|
World or Nation
|
Nation
Some moons are independent. Others fall in the jurisdiction of their planet.
All worlds and nations must follow the United Systems’ Constitution, and Bill of Rights.
Worlds under the United Systems
Roman Numerals are the Systems.
A star * represents the world of the System’s capital.
Capital letters represent Individual System Members(ISM).
Numbers are worlds under the ISM jurisdiction.
Note: Unpopulated worlds are not listed.
This list was compiled 2295. ISMs who joined the
US after 2295 are not listed.
(2295 Census) System or
Organization Human ISM Total /Year JoinedPopulation___
VI. Ross 128 US/2295 41,020
A. Ross128-1 Joint Human/Alphan(93) 38,970 39,290
1. Ross128-1c Ross/2293 320
B. *Ross128-3 Ross/2294 1,730 1,730
VII. Ross 154 US/2299 5,910
A. Ross154-2b Ross/2295 5,910 5,910
How would spring water react when exposed to Mars current environment?
It depends somewhat on the area of Mars we are talking about. In the Hellas Basin, on a warm summer day, water could exist for a long time.
But for most of Mars, here is what I think would happen.
Some of it would boil and evaporate in the thin dry Mars air and some would freeze(and evaporate later). But if the water source was large enough for the spring to stay active awhile, it would overfill the spring and flow, cutting channels as it goes. A layer of ice would form over the channel, slowing the evaporation of the water.
Once the water source was deplenished, the water would stop flowing ice covering the channel would evaporate, leaving dry channels.
The Nilosyrtis Mensae area of Mars shows many signs of water, both in the past and possibly now. There might be active springs and glaciers in this area.
The Nilosyrtis Mensae area of Mars has been a great interest of study for me for the last 5 years when I came across this picture;
[http://www.msss.com/moc_gallery/ab1_m04 … 304128.jpg]http://www.msss.com/moc_gallery/ab1_m04 … 304128.jpg
(Taken from here
[http://www.msss.com/moc_gallery/ab1_m04 … 4128.html)]http://www.msss.com/moc_gallery/ab1_m04 … 4128.html)
Look about midway down the picture and you will see what look like channels coming out of several craters.
To the south is some high lands. Any ground water would flow down into these lowlands. If such groundwater existed, it could come up in springs, where craters have punctured the surface.
Is the white material in the craters light dust, or ice?
Those channels are very puzzling.
You can also barley make out one of these channels coming out of the large crater about halfway down this picture;
[http://www.msss.com/moc_gallery/ab1_m04 … 402905.jpg]http://www.msss.com/moc_gallery/ab1_m04 … 402905.jpg
(Taken from here
[http://www.msss.com/moc_gallery/ab1_m04 … 2905.html)]http://www.msss.com/moc_gallery/ab1_m04 … 2905.html)
Shortly after I made this discovery, I informed Malin Space Science Systems. I requested that they study this area some more and was surprised to see them do this;
[http://www.msss.com/moc_gallery/e07_e12/mc13.html]http://www.msss.com/moc_gallery/e07_e12/mc13.html
and here
[http://www.msss.com/moc_gallery/m19_m23/mc13.html]http://www.msss.com/moc_gallery/m19_m23/mc13.html
Other evidence of Water
If you look toward the bottom of this picture;
[http://www.msss.com/moc_gallery/e07_e12 … 004556.jpg]http://www.msss.com/moc_gal....556.jpg
(Taken from here
[http://www.msss.com/moc_gallery/e07_e12 … 4556.html)]http://www.msss.com/moc_gallery/e07_e12 … 4556.html)
You’ll notice what looks like a layered shoreline. Many pictures from this area show a layered like shoreline.
This one has a nice peninsula and possible some ice filled craters.
[http://www.msss.com/moc_gallery/e19_r02 … 201147.jpg]http://www.msss.com/moc_gal....147.jpg
(taken from here
[http://www.msss.com/moc_gallery/e19_r02 … 1147.html)]http://www.msss.com/moc_gallery/e19_r02 … 1147.html)
Glaciers on Mars?
Directly to the north is an area that resembles glacier activity and maybe even active glaciers
In the wide area photo, look at the lower left hand corner, and you will see two bowl like features;
[http://www.msss.com/moc_gallery/e13_e18 … 01609.html]http://www.msss.com/moc_gallery/e13_e18 … 01609.html
On Earth, such features are scoop out by glacier (Skiers love them. I think they are called Circs).
Many pictures of this area show what look like lateral moraines in a flowing glacier.
[http://www.msss.com/moc_gallery/ab1_m04 … 245006.jpg]http://www.msss.com/moc_gallery/ab1_m04 … 245006.jpg
and at the bottom of this one;
[http://www.msss.com/moc_gallery/ab1_m04 … 306958.jpg]http://www.msss.com/moc_gallery/ab1_m04 … 306958.jpg
(Taken from here
[http://www.msss.com/moc_gallery/ab1_m04 … 06958.html]http://www.msss.com/moc_gallery/ab1_m04 … 06958.html
Humans have had an effect on the Earth’s climate, but then again, life has always effected the climate. Early life added oxygen to the Earth’s Atmosphere. But Mother Nature has us all beat. She has caused ice ages and warm periods. She has caused the sea level to rise and fall. One thing that has been constant about the Earth’s Climate is that it is always changing. I sometimes wonder if we really have as big of impact as we think.
As our knowledge of the Earth’s climate and weather improve, and as our technology advances, I think the human race will take control of the Earth’s climate and weather. It might come after Mars and Venus is terraformed. Sooner or later, thou, the Sun is going to get uncomfortably warmer (a normal part of its aging) and our descendants will have to do something if they want to keep the Earth habitable.
The key to controlling the Earth’s climate and weather is controlling the amount of solar radiation reaching the Earth. This can be done from orbit, using similar tools needed to terraform Venus. Perhaps some sort of solar shade that can let various amounts of sunlight through, on any given area on it.
For example, one spot on the shade is not letting any light through, to cast a shadow on a hurricane and kill it. Another part it letting 70% light through to cool off an area in a drought. Orbital lenses and mirrors might be helpful as well. An orbital lense could be used to increase water vapor by evaporating ocean water. It could also be used to warm frozen areas and to help grow crops in places like Sibera. Mirrors could also help crops by extending daylight hours over farmland.
bolbuyk, The thought of using asteroids crossed my mind, except that I wouldn’t feel comfortable with an asteroid coming that close to the Earth. If we could ensure the safety of Earth and Mars, then an asteroid would make a great cycler base/ship.
Chat, I see two ways we could build at the atomic level using the resources of a planet, asteroid or moon.
The first way is to follow the examples of a plant. A plant starts out as a seed. This seed digs roots into the ground. The root find and transport the right atoms to build a plant. A mature apple tree knows how to take atoms out of the ground to build an apple. This is all encoded on its DNA. Imagine sending seeds (Mechanical or biological) to an asteroid. This seed sends roots throughout the asteroid and starts making whatever we have programmed it to make.
The second way works a little differently to achieve the same results. Let’s build an apple, but we are not going to use DNA to tell us how to build it. Let’s map out every atom in the apple in a 3-D map. We’ll note the location and type of every atom in the apple. Then we’ll collect the atoms we need to build an exact copy (Using mechanical roots or nanobots). All that is left is to put each atom in its correct location, following the atomic map, and we have an exact copy of the atom.
To be able to send a seed to a planet, moon, or asteroid, and have it build, say a fully stocked base (or whatever we wanted) would be a tremendous step for the human race. To be able to map and build things at the atomic level would be an even greater step. Space exploration, colonization and terraforming would become so much easier.
Several of you mentioned Earth’s climate, and the good or bad of causing change. What we need to learn how to do is to control the Earth’s climate. We need to learn how to control the amount of solar radiation reaches any given point on the Earth, and exactly what effect that will have locally and globally.
This could be done with orbital mirrors, shades and lenses. Imagine being able to cut a hurricanes energy by casting a shadow on it. Or end a drought by evaporating sea water and creating rain clouds.
For long term, stopping any greenhouse threat, or ice age threat. And then there is the greatest threat to the Earth’s climate- the Sun. The Sun is slowly aging. As it gets older, it is predicted to get hotter, and eventually it will make the Earth uninhabitable. Some scientists have predicted this could start in as little as 10,000 years, while other say a million years or more(So we do not know for sure, but the Sun will get hotter as it ages).
Before the human race can take on such a risky and challenging endeavor, we need to have a greater understanding on how our weather and climate works. We are getting better, but we still can not make precise long term predictions of the weather. We’ll need to have a much greater understanding before we tamper with the cliamte. We’ll need to know thinks like, “If I keep Houston, TX at a nice 80 degrees all summer, what kind of long term effect will that have on the global climate and can I counter that effect?”
We could also learn a lot by terraforming Venus and Mars, especially Venus. Venus would be a great place to perfect controlling a global climate from orbit. We could learn a lot from Venus.
I don’t expect humans will be controlling the Earth’s weather and climate any time soon, but one day, a few hundred years from now (built on the foundation of the knowledge and experience gained over the years) humans will be in control of the solar radiation reaching the Earth. The threat of becoming too hot or too cold will be a thing for history.
First of all, has this topic been discussed before, here? I couldn't find a thread on it, but I hate to start a new one if it has.
In my story, "War Against Gravity," set 200 years in our future, the Sahara had been 'terraformed,' into a rainforest. The Gobi and central desert of Australia had also been terraformed.
To do this, orbital lenses evaporated vast amounts of sea water up wind of the deserts. Over time, dense forest grew and locked in water. Also, great aquifers were created.
Orbital lenses may not be practical. Perhaps we could turn vast amounts of sea water into freshwater (Using Solar Power, of course) and pump it to these deserts (using pipes, much like we do for oil). I believe that eventually a large rainforest would lock in water locally so that a wet climate would remain stable without having to pump in more water.
The timeframe I am envisioning is just over a hundred years to get a stable rainforest. (Maybe sooner if it was aggressively pursued)