Difference between revisions of "Tylo/cs"

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(Created page with "{{:Tylo/Data}} '''Tylo''' is the third moon of Jool. It is the largest of Jool's five moons, the largest moon in the entire Kerbol System, and the largest celesti...")
 
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{{:Tylo/Data}}
 
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'''Tylo''' is the third [[moon]] of [[Jool]]. It is the largest of Jool's five moons, the largest moon in the entire [[Kerbol System]], and the largest celestial body without an atmosphere. It is Kerbal Space Program's analog for [[w:Ganymede_(moon)|Ganymede]], a moon of [[w:Jupiter|Jupiter]].
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'''Tylo''' je třetí měsíc planety [[Jool/cs|Jool]]. Je největší měsíc Joolu i celé sluneční soustavy a také největší vesmírný objekt bez atmosféry. Jako předloha pro Tylo posloužil Ganymed, měsíc Jupitera.
  
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Landing on Tylo is extremely challenging. Its gravity is similar to [[Kerbin]]'s, but aerobraking is impossible, since there is no [[atmosphere]]. However, due to its large gravity well, Tylo is an ideal target for a [[Tutorial: Gravity Assist|gravity assist]] to enter or leave the Jool system safely and with minimal fuel consumption.
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Přistání na povrchu je extrémní výzva. Gravitace je podobná jako na [[Kerbin/cs|Kerbinu]], ale aerobraking je kvůli absenci atmosféry nemožný. Na druhou stranu, díky jeho silné gravitaci může být Tylo použit jako [[Tutorial: Gravity Assist|gravitační prak]] pro vlet nebo výlet z Jool systému s minimálními náklady na palivo.
  
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Having a spacecraft orbiting very close to the surface can give you orbit periods of about 29 minutes going about 2,170 m/s. Like the other large Joolian moons, Tylo is tidally locked. Synchronous orbits around Tylo are not possible, as they would lie outside of its SOI, at a radius of 14,758,067 meters.
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Vesmírná raketa obíhající těsně nad povrchem oběhne měsíc za 29 minut rychlostí okolo 2,170 m/s. Jako všechny další velké měsíce Joolu má Tylo vázanou rotaci s planetou. Synchronní orbita kolem měsíce je nemožná, protože potřebná výška 14,758,067 metrů je už mimo sféru vlivu.
  
 
== Topography ==
 
== Topography ==
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Tylo has a rocky surface. It has a varying elevation between 0 meters (Tylo baseline height) and peaks of more than 11290 meters.  
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Tylo má velmi hornatý povrch. Výška povrchu se pohybuje od nuly až po více než 11,290 metrů.
  
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Tylo's surface looks similar to that of [[Mün]], but has much fewer impact craters (especially on the side facing away from Jool) and is more uneven.
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Tylo's surface looks similar to that of [[Mun/cs|Mun]], but has much fewer impact craters (especially on the side facing away from Jool) and is more uneven.
 
   
 
   
 
Due to the coloring of the surface of Tylo, it is likely that it is covered in a rhyolite layer of rock, nickel, a little cobalt, some sort of ice and dust, spread by meteorite impacts.
 
Due to the coloring of the surface of Tylo, it is likely that it is covered in a rhyolite layer of rock, nickel, a little cobalt, some sort of ice and dust, spread by meteorite impacts.

Revision as of 18:26, 6 August 2013

Tylo/Data

Tylo je třetí měsíc planety Jool. Je největší měsíc Joolu i celé sluneční soustavy a také největší vesmírný objekt bez atmosféry. Jako předloha pro Tylo posloužil Ganymed, měsíc Jupitera.

Přistání na povrchu je extrémní výzva. Gravitace je podobná jako na Kerbinu, ale aerobraking je kvůli absenci atmosféry nemožný. Na druhou stranu, díky jeho silné gravitaci může být Tylo použit jako gravitační prak pro vlet nebo výlet z Jool systému s minimálními náklady na palivo.

Vesmírná raketa obíhající těsně nad povrchem oběhne měsíc za 29 minut rychlostí okolo 2,170 m/s. Jako všechny další velké měsíce Joolu má Tylo vázanou rotaci s planetou. Synchronní orbita kolem měsíce je nemožná, protože potřebná výška 14,758,067 metrů je už mimo sféru vlivu.

Topography

Tylo má velmi hornatý povrch. Výška povrchu se pohybuje od nuly až po více než 11,290 metrů.

Tylo's surface looks similar to that of Mun, but has much fewer impact craters (especially on the side facing away from Jool) and is more uneven.

Due to the coloring of the surface of Tylo, it is likely that it is covered in a rhyolite layer of rock, nickel, a little cobalt, some sort of ice and dust, spread by meteorite impacts. Although very large in comparison to other moons, it is unlikely that it is a captured planet. For a planet of this size, Jool would have to be much larger and denser to produce a large and strong enough gravitational well. It is a mystery why Tylo hasn't formed an atmosphere.

Because of it's high gravity and lack of an atmosphere, Tylo is very hard to land on and reach orbit from. However, low altitude orbits at high speeds can be achieved for these same reasons.

Reference Frames

Time warp Minimum Altitude
1× Any
5× 30 000 m
10× 30 000 m
50× 60 000 m
100× 120 000 m
1 000× 240 000 m
10 000× 480 000 m
100 000× 600 000 m

Trivia

  • Kerbin has the same equatorial radius as Tylo (600,000m) yet Tylo's surface gravity is much lower than Kerbin. This is most likely because Tylo is composed of low density matter.
  • There are two known Easter eggs on Tylo. One is Carl Sagan's face on a mountain and the other is a cave-like underground formation.

Gallery

  • Topographical map of Tylo.

  • Gui Tylo Polars Topo.png

  • A topographic height map of Tylo made with the ISA MapSat plugin

  • Picture of Tylo as seen from Laythe

  • A Joolrise with a Laythe transit seen from a very low orbit around Tylo

  • A small crater on Tylo as seen from the surface

Changes

0.17
  • Initial Release
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