Difference between revisions of "Duna"

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{{Infobox/Body}}
 
{{Infobox/Body}}
  
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'''Duna''' is the fourth planet of the [[Kerbol System|Kerbol star system]] and [[w:Mars|Mars]] analog for Kerbal Space Program. It is mostly red with polar icecaps and has one natural satellite, the [[moon]] '''[[Ike]]'''. Ike's size and proximity tidally locks it and Duna to each other.
+
'''Duna''' is the fourth planet from [[Kerbol]] and the fourth-largest planet. It is the [[w:Mars|Mars]] analog for Kerbal Space Program. It has one tidally-locked and large natural satellite, the [[moon]] [[Ike]]. Duna is a terrestrial planet with a red-brown surface and polar ice caps similar to that of [[Kerbin]].  
  
−
With proper [[aerobraking]], a round trip from [[Kerbin]] to Duna's [[orbit]] and back requires roughly 1700 m/s of [[Terminology#Physics|delta-v]], less than a round trip to any other planet. Duna is often the easiest planet to [[encounter]] because its orbital inclination is low.
+
Duna's orbit has nearly the same inclination as Kerbin around Kerbol, making the planet one of the easiest to [[encounter]].  If the planets align properly, using a ballistic insertion burn from 100km, with proper [[aerobraking]], a round trip from Kerbin to [[orbit]] around Duna and back requires ~1700 m/s of LKO [[Terminology#Physics|delta-v]], a relatively low amount compared to other interplanetary destinations. The trip may require a considerably higher delta-v budget for different orientations of Kerbin and Duna.
  
−
There is a [[tutorial]] about [[Tutorial:How to get to Duna|Traveling to Duna and Back]].
+
A [[Tutorial:How to get to Duna|tutorial to get to Duna]] is available at the link.
  
 
== In-game description ==
 
== In-game description ==
  
 +
'''KSP 1:'''
 
{{Quote
 
{{Quote
 +
|Also known as the red dot that you can see if you squint at it really hard, Duna has long been a wonder to Kerbalkind. The planet has been held in much awe, due to its striking red color and stark contrast to the color green.
 +
|[[Kerbal Astronomical Society]]}}
  
−
|Also known as the red dot that you can see if you squint at it really hard, Duna has long been a wonder to Kerbalkind. <br><br> The planet has been held in much awe due to its striking red color and stark contrast to the color green.
+
'''KSP 2:'''
−
 
+
{{Quote
−
|[[Kerbal Astronomical Society]]}}
+
|Duna, The Reddest Planet, has long been an object of study and inspiration to Kerbal scientists and artists alike! Its thin, low-pressure atmosphere allows for both aerobraking and relatively easy access to its surface. Kerbal researches and sci-fi writers often discuss the discoveries that could be waiting for them in the planet's polar ice caps or on Duna's tidally locked moon, Ike.|}}
  
 
== Topography ==
 
== Topography ==
−
[[File:Duna Topo ISA 3200x1600 compressed.png|thumb|left|A topographic map of Duna made with the ISA MapSat plugin]]
+
[[File:Duna_heightmap_2018.png|thumb|left|A topographic map of Duna obtained with the Kittopia mod (2018)]]
 
Duna's terrain ranges in altitude from 124 to 8264 meters. Its mountain ranges are a peril to landing [[craft]], due to their steepness and the limited [[aerobraking]] that is possible in Duna's tenuous [[atmosphere]] at such altitudes.
 
Duna's terrain ranges in altitude from 124 to 8264 meters. Its mountain ranges are a peril to landing [[craft]], due to their steepness and the limited [[aerobraking]] that is possible in Duna's tenuous [[atmosphere]] at such altitudes.
  
 
Duna has several craters. They appear quite eroded, presumably by the wind.
 
Duna has several craters. They appear quite eroded, presumably by the wind.
  
−
Several [[w:Lunar maria|maria]] (large regions of dark soil) are around several hundred meters altitude. Their low altitude allows for more aerobraking, and the flatness of the terrain makes them easy but boring landing locations. These may have been lakes when the planet may have had liquid on its surface in the past.
+
Several [[w:Lunar maria|maria]] (large regions of dark soil) are around several hundred meters altitude. Their low altitude allows for more aerobraking, and the flatness of the terrain makes them easy but boring landing locations. These may have been lakes when the planet may have had liquid on its surface in the past.
  
−
Duna's surface contains 3 [[List of easter eggs#Duna|anomalous features]].
+
Duna's surface contains 5 [[List of easter eggs#Duna|anomalous features]].
  
 
== Biomes==
 
== Biomes==
−
Duna has 5 [[biome]]s.
+
 
 +
Duna has 14 [[Biome]]s. Within the generic mix of Low-, Mid- and Highlands lie various Basins and Canyons with some scattered craters. The most dominant feature is the Midland Sea,<ref>Not a real sea. For real seas, see [[Kerbin]], [[Laythe]], [[Eve]].</ref> which spans half the Planet. The Poles also include separate Highlands and Craters.
  
 
=== Biome list ===
 
=== Biome list ===
 
{{Biome list|
 
{{Biome list|
 
* Poles
 
* Poles
 +
* Polar Highlands
 +
* Polar Craters
 
* Highlands
 
* Highlands
 
* Midlands
 
* Midlands
 
* Lowlands
 
* Lowlands
−
* Craters (Currently found in the border of poles, not actually in "craters").
+
* Craters
−
}}
+
* Midland Sea
 +
* Northeast Basin
 +
* Southern Basin
 +
* Northern Shelf
 +
* Midland Canyon
 +
* Eastern Canyon
 +
* Western Canyon}}
 +
 
 +
[[File:DunaBiomeMap.png|thumb|none|Duna biome map (legend)]]
 +
 
 +
== KSP2 ==
 +
 
 +
=== Research Orbital Boundaries ===
 +
.
 +
{| class="wikitable"
 +
|-
 +
! Boundary !! Altitude
 +
|-
 +
| Atmosphere || 0 - 49 999 m
 +
|-
 +
| Low Orbit || 50 000 m - 69 999 m
 +
|-
 +
| High Orbit || 70 000 m - 47 921 949 m
 +
|}
 +
 
 +
=== Surface Research Locations ===
 +
Surface research locations on Duna include:
 +
 
 +
* Highlands
 +
* Lowlands
 +
* Midlands
 +
* Monument
 +
* Polar Deserts
 +
* North Pole
 +
* South Pole
 +
 
 +
=== Maps ===
 +
==== Biomes ====
 +
[[File:duna_region_ui.jpg|thumb|none|Duna biome map with legend (as of v0.2.1.0 (from Orbital Survay mod))]]
 +
[https://i.imgur.com/gCZ83i6.jpeg Duna biome map (Imgur)]
 +
 
 +
==== Visual map ====
 +
[[File:duna_visual.png|thumb|none|Duna visual map (as of v0.2.1.0)]]
 +
[https://i.imgur.com/45o0hZ1.png Duna visual map (Imgur)]
  
 
== Atmosphere ==
 
== Atmosphere ==
 
[[File:Duna_Atmosphere_T&P.png|thumbnail|left|Temperature and pressure of Duna's atmosphere as a function of altitude.]]
 
[[File:Duna_Atmosphere_T&P.png|thumbnail|left|Temperature and pressure of Duna's atmosphere as a function of altitude.]]
  
−
Duna has a thin, cool [[atmosphere]] with a mass of approximately 3.0×10<sup>15</sup> kilograms, a datum level pressure of 6.755 kilopascals (0.067 atmosphere), and a depth of 50,000 meters. Compared to the atmosphere of [[Kerbin]], Duna's atmosphere has 1/15<sup>th</sup> the mass, 1/15<sup>th</sup> the surface pressure, and 1/9<sup>th</sup> the surface density. The datum level pressure on Duna is equivalent to that at an altitude of 14,975 m on Kerbin. The pressure at the top of Duna's highest mountain peak is only 2.4 kPa.
+
Duna has a thin, cool [[atmosphere]] with a mass of approximately 3.0×10<sup>15</sup> kilograms, a datum level pressure of 6.755 kilopascals (0.067 atmosphere), and a depth of 50,000 meters. Compared to the atmosphere of [[Kerbin]], Duna's atmosphere has 1/15<sup>th</sup> the mass, 1/15<sup>th</sup> the surface pressure, and 1/9<sup>th</sup> the surface density. The datum level pressure on Duna is equivalent to that at an altitude of 14,975 m on Kerbin. The pressure at the top of Duna's highest mountain peak is only 2.4 kPa.
  
−
The average [[w:Molecular_mass|molecular weight]] of Duna air is 42 g/mol, and its [[w:Heat_capacity_ratio|adiabatic index]] is 1.20. Although the composition of Duna's atmosphere is unknown, these values suggest that it may consist largely of [[w:Carbon_dioxide|carbon dioxide]].
+
The average [[w:Molecular_mass|molecular weight]] of Duna air is 42 g/mol, and its [[w:Heat_capacity_ratio|adiabatic index]] is 1.20. Although the composition of Duna's atmosphere is unknown, these values suggest that it may consist largely of [[w:Carbon_dioxide|carbon dioxide]].
  
−
Like all other atmospheres in the game, Duna's atmosphere fades exponentially as altitude increases. The [[w:Scale_height|scale height]] varies with altitude, which is a change from pre-1.0 [[Version_history|versions]] of the game. The pressure-altitude profile is globally constant and independent of temperature. The following table gives the atmospheric pressure at various altitudes above the datum level.
+
Like all other atmospheres in the game, Duna's atmosphere fades exponentially as altitude increases. The [[w:Scale_height|scale height]] varies with altitude, which is a change from pre-1.0 [[Version_history|versions]] of the game. The pressure-altitude profile is globally constant and independent of temperature. The following table gives the atmospheric pressure at various altitudes above the datum level.
  
 
{| class="wikitable"
 
{| class="wikitable"
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|}
 
|}
  
−
The surface of Duna is cold, with a globally averaged datum level temperature of approximately -23 °C. Air temperatures decrease with increasing altitude to an altitude of 30 km. Between the altitudes of 30-45 km lies an isothermal layer, having a temperature of -123 °C.
+
The surface of Duna is cold, with a globally averaged datum level temperature of approximately -23 °C. Air temperatures decrease with increasing altitude to an altitude of 30 km. Between the altitudes of 30-45 km lies an isothermal layer, having a temperature of -123 °C.
  
−
Air temperatures vary with latitude and time of day. At the equator, datum level temperatures vary between a nighttime low of -20 °C and a daytime high of -2 °C. At the poles, the temperature varies between -90 °C and -85 °C. Since Duna has no axial tilt, there are no seasonal temperature variations.
+
Air temperatures vary with latitude and time of day. At the equator, datum level temperatures vary between a nighttime low of -20 °C and a daytime high of -2 °C. At the poles, the temperature varies between -90 °C and -85 °C. Since Duna has no axial tilt, there are no seasonal temperature variations.
  
 
[[File:Duna north pole.png|thumb|right|200px|Duna's north pole]]
 
[[File:Duna north pole.png|thumb|right|200px|Duna's north pole]]
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=== Atmospheric flight ===
 
=== Atmospheric flight ===
−
The thickness of Duna's atmosphere makes it suitable for [[aerobraking]] from a high-speed interplanetary intercept. The periapsis altitude required for a successful aerocapture depends on the spacecraft's drag characteristics, its approach velocity, and the desired apoapsis of the resulting orbit. For an intercept originating from Kerbin, it appears that, under most conditions, the intercept periapsis should be about 17±7 km.
+
The thickness of Duna's atmosphere makes it suitable for [[aerobraking|aerocapture]] from a high-speed interplanetary intercept. The periapsis altitude required for a successful aerocapture depends on the spacecraft's drag characteristics, its approach velocity, and the desired apoapsis of the resulting orbit. The most effective periapsis for aerocapture is best determined experimentally; however, for a Hohmann transfer originating from Kerbin, it appears that the target range lies between 10 km and 20 km.
  
−
Although [[parachute]]s will deploy on Duna, the atmosphere is so thin that they are usually unable to slow a craft to a safe landing velocity and must be assisted with engines. Parachute performance can be particularly troubling when attempting to land in highland areas. Attaining the same vehicle descent rate on Duna that a vehicle would have on Kerbin requires about 2.5 times the parachute area.  
+
Although [[parachute]]s will deploy on Duna, the atmosphere is so thin that they are usually unable to slow a craft to a safe landing velocity and must be assisted with engines. Parachute performance can be particularly troubling when attempting to land in highland areas. Attaining the same vehicle descent rate on Duna that a vehicle would have on Kerbin requires about 2.5 times the parachute area.  
  
 
Below 5 km Duna's atmosphere is thick enough to allow wings to generate enough lift for aerodynamic flight. Jet engines don't work for want of oxygen, but other propulsion methods work well. Performing a horizontal landing with a plane is also possible.  
 
Below 5 km Duna's atmosphere is thick enough to allow wings to generate enough lift for aerodynamic flight. Jet engines don't work for want of oxygen, but other propulsion methods work well. Performing a horizontal landing with a plane is also possible.  
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== Observation of Ike ==
 
== Observation of Ike ==
 
{{gif image|Ikes_libration.gif|thumb|An animation of an orbit viewed from Duna|width=304|float=left|additional css=margin-right:1em;margin-bottom:1em}}
 
{{gif image|Ikes_libration.gif|thumb|An animation of an orbit viewed from Duna|width=304|float=left|additional css=margin-right:1em;margin-bottom:1em}}
−
Ike's orbit keeps it directly above a short range of Dunar longitudes. The average Duna longitude that Ike tends to stay directly above (at the [[w:Zenith|Zenith]]) is 6 degrees east, but the eccentricity of Ike's orbit causes the exact longitude to oscillate between about 2 degrees and 10 degrees east and makes Ike appear to grow slightly larger and smaller to an observer on the surface of Duna. The latitude at which Ike is in the Zenith also oscillates between 0.2 degrees south and 0.2 degrees north due to Ike's orbital inclination, making Ike appear to rotate upwards and downwards as viewed from the surface, but due to the extremely small orbital inclination, this effect is nearly imperceptible. These phenomena together are known as [[w:libration|libration]]. The oscillation in Ike's position above the horizon allows areas from 88°W to 80°W and 92°E to 100°E on Duna to observe Ike rise and set at least partially across the horizon, as can any areas north of 89.8°N or south of 89.8°S.
+
Ike's orbit keeps it directly above a short range of Dunaian longitudes. The average Duna longitude that Ike tends to stay directly above (at the [[w:Zenith|Zenith]]) is 6 degrees east, but the eccentricity of Ike's orbit causes the exact longitude to oscillate between about 2 degrees and 10 degrees east and makes Ike appear to grow slightly larger and smaller to an observer on the surface of Duna. The latitude at which Ike is in the Zenith also oscillates between 0.2 degrees south and 0.2 degrees north due to Ike's orbital inclination, making Ike appear to rotate upwards and downwards as viewed from the surface, but due to the extremely small orbital inclination, this effect is nearly imperceptible. These phenomena together are known as [[w:libration|libration]]. The oscillation in Ike's position above the horizon allows areas from 88°W to 80°W and 92°E to 100°E on Duna to observe Ike rise and set at least partially across the horizon, as can any areas north of 89.8°N or south of 89.8°S.
  
 
== Interplanetary travel ==
 
== Interplanetary travel ==
  
−
From altitude orbit around Duna, the delta-V needed to reach the orbits of other celestials is:
+
From a 60 km altitude orbit around Duna, the requirements for attaining an intercept trajectory of other celestials are:
  
 
{| class="wikitable"
 
{| class="wikitable"
 
!Body
 
!Body
−
!colspan="2"|Delta-V
+
!Delta-V<ref>[http://www.dcl.hpi.uni-potsdam.de/home/feinbube/web/stealth/KSPDeltaVMap/ KSP Delta V Planner]</ref>
 +
!Phase Angle<ref>[http://ksp.olex.biz/ Transfer calculator]</ref>
 
|-
 
|-
 
| [[Ike]]
 
| [[Ike]]
−
|colspan="2"| ~300&nbsp;m/s
+
|align="right"| ~360&nbsp;m/s
 +
|align="right"| N/A
 
|-
 
|-
 
| [[Kerbin]]
 
| [[Kerbin]]
−
|colspan="2"| ~620&nbsp;m/s
+
|align="right"| ~810&nbsp;m/s
 +
|align="right"| -75º
 +
|-
 +
| [[Eve]]
 +
|align="right"| ~910&nbsp;m/s
 +
|align="right"| -169º
 
|-
 
|-
 
| [[Dres]]
 
| [[Dres]]
−
|colspan="2"| ~820&nbsp;m/s
+
|align="right"| ~1200&nbsp;m/s
 +
|align="right"| 62º
 
|-
 
|-
−
| [[Eve]]
+
| [[Jool]]
−
|colspan="2"| ~1080&nbsp;m/s
+
|align="right"| ~1610&nbsp;m/s
 +
|align="right"| 86º
 
|-
 
|-
−
| [[Jool]]
+
| [[Moho]]
−
|colspan="2"| ~1350&nbsp;m/s
+
|align="right"| ~1650&nbsp;m/s
 +
|align="right"| -158º
 
|-
 
|-
 
| [[Eeloo]]
 
| [[Eeloo]]
−
|colspan="2"| ~1580&nbsp;m/s
+
|align="right"| ~1780&nbsp;m/s
−
|-
+
|align="right"| 93º
−
 
 
−
| [[Moho]]
 
−
|colspan="2"| ~2100&nbsp;m/s
 
 
|-
 
|-
 
|}
 
|}
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File:Parachute_Descent.png|Parachute descent down to Duna surface.  
 
File:Parachute_Descent.png|Parachute descent down to Duna surface.  
 
File:ISA_over_Duna.png|ISA satellite in orbit over Duna being used to map the planet surface.
 
File:ISA_over_Duna.png|ISA satellite in orbit over Duna being used to map the planet surface.
−
File:DunaSurface.png|Duna's surface at Dawn.
+
File:Kerbal Space Program Enhanced Edition 20211225182926.jpg|A small unmanned rover just saw some surface "blueberries"!
 +
File:DunaSurface.png|Duna's surface at dawn.
 
File:Duna_and_ike.jpg|Duna and Ike.
 
File:Duna_and_ike.jpg|Duna and Ike.
−
File:Duna_map_800.gif|A topographic height map of Duna made with the ISA MapSat plugin.
+
File:Duna_map_800.gif|A pre-0.21 topographic height map of Duna made with the ISA MapSat plugin.
−
File:DoonaMap.png|A color map of Duna.
+
File:DoonaMap.png|A pre-0.21 color map of Duna.
 
File:North pole of Duna.jpg|A lander on the northern pole of Duna.
 
File:North pole of Duna.jpg|A lander on the northern pole of Duna.
 
File:Duna_Sunrise.png|Duna at [http://www.youtube.com/watch?v=7czFsEpe4Ww&feature=youtu.be sunrise].
 
File:Duna_Sunrise.png|Duna at [http://www.youtube.com/watch?v=7czFsEpe4Ww&feature=youtu.be sunrise].
 
File:Duna-sinkhole.png|A rover at the edge of one of the "sinkholes."
 
File:Duna-sinkhole.png|A rover at the edge of one of the "sinkholes."
−
File:Thepoopscooperduna1.png|Bill, his capsule, a flag, and Ike are all in this picture.
 
−
File:TakeoffFromDunaV21.1.png|A small probe after takeoff, climbing into a low orbit around Duna.
 
 
File:OrbitingDunaV21.1.png|A small probe orbiting Duna.
 
File:OrbitingDunaV21.1.png|A small probe orbiting Duna.
 
File:Duna_Ike_Eclipse.png|Ike partially eclipsing Kerbol. Note the dimmer light and the solar panels not charging.
 
File:Duna_Ike_Eclipse.png|Ike partially eclipsing Kerbol. Note the dimmer light and the solar panels not charging.
 
File:Duna from ike.png| Duna seen from Ike.
 
File:Duna from ike.png| Duna seen from Ike.
−
File:DunaExplorer.png |Peter Kerman exploring the surface of Duna with a nice view on Kerbol, Ike, and the lander.
 
 
File:DunaSpaceTlscope.png|Duna and Ike as seen from a space telescope.
 
File:DunaSpaceTlscope.png|Duna and Ike as seen from a space telescope.
−
File:Duna Landing.png|A three Kerbal lander on Duna.
+
File:duna lander tipped over.png|The road to Duna is paved with speedbumps...
 +
File:ikerise.png|...but the journey is worth the effort!
 +
File:Duna rover.jpg|A rover on the surface of duna.
 
</gallery>
 
</gallery>
  
−
== Changes ==
+
== Changes KSP1 ==
 +
;[[1.2]]
 +
* Added biomes
 
;[[1.0.5]]
 
;[[1.0.5]]
 
* Changed atmosphere characteristics
 
* Changed atmosphere characteristics
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;[[0.17]]
 
;[[0.17]]
 
* Initial Release
 
* Initial Release
 +
 +
== Changes KSP2 ==
 +
;[[KSP2 v0.2.0.0]]
 +
* Added research locations
  
 
== Trivia ==
 
== Trivia ==
−
* According to former developer NovaSilisko, Duna's appearance was inspired by the theory that ice ages on Mars may have brought the ice caps much closer to its equator. <ref>[http://forum.kerbalspaceprogram.com/threads/96153-Duna-s-ice-caps-are-too-big?p=1465456&viewfull=1#post1465456 NovaSilisko's] answer in “Duna's ice caps are too big”.</ref>
+
[[File:EgarAndMeander.jpg|thumb|right|Egar in orbit of Meander]]
−
* Duna's name may be either a reference to its desert landscape or a reference to the [[w:Frank Herbert|Frank Herbert]] novel ''[[w:Dune (novel)|Dune]]''.
+
* Duna was originally called "Egar" and was in orbit of Meander, the precursor of [[Jool]]. It was described as half icy wasteland, half desert. <ref>[http://forum.kerbalspaceprogram.com/index.php?/topic/1850-a-kerbals-guide-to-our-solar-system/ Kerbol System Proposal in the forum by NovaSilisko, Aug 2011]</ref>
 +
* According to former developer NovaSilisko, Duna's appearance was inspired by the theory that ice ages on Mars may have brought the ice caps much closer to its equator. - Meaning that Duna might be in a ice age. <ref>[https://forum.kerbalspaceprogram.com/topic/86696-dunas-ice-caps-are-too-big/#comment-1451461 NovaSilisko's] answer in “Duna's ice caps are too big”.</ref>
 +
* Duna's name, which is the Spanish word for dune, may be either a reference to its desert landscape or a reference to the [[w:Frank Herbert|Frank Herbert]] novel ''[[w:Dune (novel)|Dune]]''.
 
* The low-lying areas near Duna's equator make a shape resembling Europe.
 
* The low-lying areas near Duna's equator make a shape resembling Europe.
 
{{SpoilerBox
 
{{SpoilerBox
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* On the surface of Duna, there is a large monument carved in the likeness of a [[List of easter eggs#Duna|Kerbal face]], alluding to the infamous "Face of Mars" discovered in the Cydonia Mensae region of Mars during the 1970's.  
 
* On the surface of Duna, there is a large monument carved in the likeness of a [[List of easter eggs#Duna|Kerbal face]], alluding to the infamous "Face of Mars" discovered in the Cydonia Mensae region of Mars during the 1970's.  
 
* Buried deep under the surface, there is a small camera, similar to the design on the [[w:Curiosity (rover)|Curiosity]] rover.
 
* Buried deep under the surface, there is a small camera, similar to the design on the [[w:Curiosity (rover)|Curiosity]] rover.
−
* One anomalous feature on Duna is a small, pyramid-like hill emitting an SSTV signal. When decrypted, it shows a diagram-like image of three figures standing next to the hill itself, implying that Duna was once inhabited or visited before.
+
* One anomalous feature on Duna is a small, pyramid-like hill emitting an SSTV signal. When decrypted, it shows a diagram-like image of three figures standing next to the hill itself, which was originally part of the developer's story but later scrapped.
 +
* There is a stranded rover on Duna which appears similar to the NASA Spirit and Opportunity rovers.
 +
* There is one randomly generated green monolith on Duna.
 
}}
 
}}
−
* It may be possible to reach Duna by year 1, day 2 by launching immediately with a delta-v of over 2 million m/s
+
* It may be possible to reach Duna by year 1, day 2(The next [[Time|Kerbin Day]]) by launching immediately with a delta-v of over 2 million m/s.
−
== Notes ==
+
** Duna's color map uses some details that are blended in from the old Duna color map (as well as procedural PQSLandControl coloration) however, this color map is from the old version of Duna, before its "revamp" in 0.21. The color map references features which no longer exist on Duna, and is offset by about 180 degrees longitude.
 +
 
 +
== References & Notes ==
 
<references />
 
<references />
  

Revision as of 18:56, 20 March 2024

Duna
Duna
Duna as seen from orbit.
Planet of Kerbol
Orbital Characteristics
Semi-major axis 20 726 155 264 m [Note 1]
Apoapsis 21 783 189 163 m [Note 1]
Periapsis 19 669 121 365 m [Note 1]
Orbital eccentricity 0.051
Orbital inclination 0.06 °
Argument of periapsis 0 °
Longitude of the ascending node 135.5 °
Mean anomaly 3.14 rad (at 0s UT)
Sidereal orbital period 17 315 400 s
801 d 3 h 50 m 0.1 s
Synodic orbital period 19 645 697.3 s
Orbital velocity 7 147 - 7 915 m/s
Physical Characteristics
Equatorial radius 320 000 m
Equatorial circumference 2 010 619 m
Surface area 1.2867964×1012 m2
Mass 4.5154270×1021 kg
Standard gravitational parameter 3.0136321×1011 m3/s2
Density 32 897.302 kg/m3
Surface gravity 2.94 m/s2 (0.3 g)
Escape velocity 1 372.41 m/s
Sidereal rotation period 65 517.859 s
3 d 0 h 11 m 57.9 s
Solar day 65 766.707 s
3 d 0 h 16 m 6.7 s
Sidereal rotational velocity 30.688 m/s
Synchronous orbit 2 880.00 km
Sphere of influence 47 921 949 m [Note 1]
Atmospheric Characteristics
Atmosphere present Yes
Atmospheric pressure 6.75500 kPa
0.066667 atm
Atmospheric height 50 000 m
6.7×10-8 atm
Temperaturemin -123.15 °C 150 K
Temperaturemax -40.15 °C 233 K
Oxygen present No
Scientific multiplier
Surface 8
Splashed N/A
Lower atmosphere 5
Upper atmosphere 5
Near space 7
Outer space 5
Recovery 5
  1. ↑ 1.0 1.1 1.2 1.3 The distances are given from the body's center, not from the surface (unlike ingame)

Duna is the fourth planet from Kerbol and the fourth-largest planet. It is the Mars analog for Kerbal Space Program. It has one tidally-locked and large natural satellite, the moon Ike. Duna is a terrestrial planet with a red-brown surface and polar ice caps similar to that of Kerbin.

Duna's orbit has nearly the same inclination as Kerbin around Kerbol, making the planet one of the easiest to encounter. If the planets align properly, using a ballistic insertion burn from 100km, with proper aerobraking, a round trip from Kerbin to orbit around Duna and back requires ~1700 m/s of LKO delta-v, a relatively low amount compared to other interplanetary destinations. The trip may require a considerably higher delta-v budget for different orientations of Kerbin and Duna.

A tutorial to get to Duna is available at the link.

In-game description

KSP 1:

“ Also known as the red dot that you can see if you squint at it really hard, Duna has long been a wonder to Kerbalkind. The planet has been held in much awe, due to its striking red color and stark contrast to the color green.

— Kerbal Astronomical Society

 ”

KSP 2:

“ Duna, The Reddest Planet, has long been an object of study and inspiration to Kerbal scientists and artists alike! Its thin, low-pressure atmosphere allows for both aerobraking and relatively easy access to its surface. Kerbal researches and sci-fi writers often discuss the discoveries that could be waiting for them in the planet's polar ice caps or on Duna's tidally locked moon, Ike. ”

Topography

A topographic map of Duna obtained with the Kittopia mod (2018)

Duna's terrain ranges in altitude from 124 to 8264 meters. Its mountain ranges are a peril to landing craft, due to their steepness and the limited aerobraking that is possible in Duna's tenuous atmosphere at such altitudes.

Duna has several craters. They appear quite eroded, presumably by the wind.

Several maria (large regions of dark soil) are around several hundred meters altitude. Their low altitude allows for more aerobraking, and the flatness of the terrain makes them easy but boring landing locations. These may have been lakes when the planet may have had liquid on its surface in the past.

Duna's surface contains 5 anomalous features.

Biomes

Duna has 14 Biomes. Within the generic mix of Low-, Mid- and Highlands lie various Basins and Canyons with some scattered craters. The most dominant feature is the Midland Sea,[1] which spans half the Planet. The Poles also include separate Highlands and Craters.

Biome list

Duna In-game biome map as of 1.2
  • Poles
  • Polar Highlands
  • Polar Craters
  • Highlands
  • Midlands
  • Lowlands
  • Craters
  • Midland Sea
  • Northeast Basin
  • Southern Basin
  • Northern Shelf
  • Midland Canyon
  • Eastern Canyon
  • Western Canyon
Duna biome map (legend)

KSP2

Research Orbital Boundaries

.

Boundary Altitude
Atmosphere 0 - 49 999 m
Low Orbit 50 000 m - 69 999 m
High Orbit 70 000 m - 47 921 949 m

Surface Research Locations

Surface research locations on Duna include:

  • Highlands
  • Lowlands
  • Midlands
  • Monument
  • Polar Deserts
  • North Pole
  • South Pole

Maps

Biomes

File:Duna region ui.jpg
Duna biome map with legend (as of v0.2.1.0 (from Orbital Survay mod))

Duna biome map (Imgur)

Visual map

File:Duna visual.png
Duna visual map (as of v0.2.1.0)

Duna visual map (Imgur)

Atmosphere

Temperature and pressure of Duna's atmosphere as a function of altitude.

Duna has a thin, cool atmosphere with a mass of approximately 3.0×1015 kilograms, a datum level pressure of 6.755 kilopascals (0.067 atmosphere), and a depth of 50,000 meters. Compared to the atmosphere of Kerbin, Duna's atmosphere has 1/15th the mass, 1/15th the surface pressure, and 1/9th the surface density. The datum level pressure on Duna is equivalent to that at an altitude of 14,975 m on Kerbin. The pressure at the top of Duna's highest mountain peak is only 2.4 kPa.

The average molecular weight of Duna air is 42 g/mol, and its adiabatic index is 1.20. Although the composition of Duna's atmosphere is unknown, these values suggest that it may consist largely of carbon dioxide.

Like all other atmospheres in the game, Duna's atmosphere fades exponentially as altitude increases. The scale height varies with altitude, which is a change from pre-1.0 versions of the game. The pressure-altitude profile is globally constant and independent of temperature. The following table gives the atmospheric pressure at various altitudes above the datum level.

Altitude (m) Pressure (Pa) Pressure (atm)
0 6 755 0.067
2 500 5 136 0.051
5 000 3 774 0.037
7 500 2 663 0.026
10 000 1 797 0.018
15 000 716.9 0.007
20 000 241.0 0.002
25 000 91.73 0.001
30 000 32.90 0.000
40 000 4.918 0.000
50 000 0 0.000

The surface of Duna is cold, with a globally averaged datum level temperature of approximately -23 °C. Air temperatures decrease with increasing altitude to an altitude of 30 km. Between the altitudes of 30-45 km lies an isothermal layer, having a temperature of -123 °C.

Air temperatures vary with latitude and time of day. At the equator, datum level temperatures vary between a nighttime low of -20 °C and a daytime high of -2 °C. At the poles, the temperature varies between -90 °C and -85 °C. Since Duna has no axial tilt, there are no seasonal temperature variations.

Duna's north pole

Duna's atmosphere appears to have a reddish or brownish color, both from the surface and from space. The atmosphere has this color even over the poles, where the surface is white.

Atmospheric flight

The thickness of Duna's atmosphere makes it suitable for aerocapture from a high-speed interplanetary intercept. The periapsis altitude required for a successful aerocapture depends on the spacecraft's drag characteristics, its approach velocity, and the desired apoapsis of the resulting orbit. The most effective periapsis for aerocapture is best determined experimentally; however, for a Hohmann transfer originating from Kerbin, it appears that the target range lies between 10 km and 20 km.

Although parachutes will deploy on Duna, the atmosphere is so thin that they are usually unable to slow a craft to a safe landing velocity and must be assisted with engines. Parachute performance can be particularly troubling when attempting to land in highland areas. Attaining the same vehicle descent rate on Duna that a vehicle would have on Kerbin requires about 2.5 times the parachute area.

Below 5 km Duna's atmosphere is thick enough to allow wings to generate enough lift for aerodynamic flight. Jet engines don't work for want of oxygen, but other propulsion methods work well. Performing a horizontal landing with a plane is also possible.

An ascent to low Duna orbit from the surface typically requires around 1400 m/s in Δv to reach a 55 km altitude traveling at roughly 900 m/s.

Orbital statistics

The synchronous orbit of Duna is at an altitude of 2 880.00 km above Duna. The speed of the satellite is 306.88 m/s and it has an orbital period resonating with 1 Duna day (18.2 hours or 65517.859375 seconds). However, this is the same altitude at which Ike orbits, so unless a ship's orbit is perfectly precise, it will eventually be captured by Ike.

For a semi-synchronous orbit of ½ Duna day (9.1 hours or 32758.9295 seconds) an orbit of 1 695.87 km above Duna is needed with a velocity of 386.65 m/s.

Observation of Ike

Ikes libration.gif
An animation of an orbit viewed from Duna

Ike's orbit keeps it directly above a short range of Dunaian longitudes. The average Duna longitude that Ike tends to stay directly above (at the Zenith) is 6 degrees east, but the eccentricity of Ike's orbit causes the exact longitude to oscillate between about 2 degrees and 10 degrees east and makes Ike appear to grow slightly larger and smaller to an observer on the surface of Duna. The latitude at which Ike is in the Zenith also oscillates between 0.2 degrees south and 0.2 degrees north due to Ike's orbital inclination, making Ike appear to rotate upwards and downwards as viewed from the surface, but due to the extremely small orbital inclination, this effect is nearly imperceptible. These phenomena together are known as libration. The oscillation in Ike's position above the horizon allows areas from 88°W to 80°W and 92°E to 100°E on Duna to observe Ike rise and set at least partially across the horizon, as can any areas north of 89.8°N or south of 89.8°S.

Interplanetary travel

From a 60 km altitude orbit around Duna, the requirements for attaining an intercept trajectory of other celestials are:

Body Delta-V[2] Phase Angle[3]
Ike ~360 m/s N/A
Kerbin ~810 m/s -75º
Eve ~910 m/s -169º
Dres ~1200 m/s 62º
Jool ~1610 m/s 86º
Moho ~1650 m/s -158º
Eeloo ~1780 m/s 93º

Reference frames

Time warp Minimum Altitude
1× Any
5× 50 000 m (above the atmosphere)
10× 50 000 m (above the atmosphere)
50× 60 000 m
100× 100 000 m
1 000× 300 000 m
10 000× 600 000 m
100 000× 800 000 m

Gallery

  • Parachute descent down to Duna surface.

  • ISA satellite in orbit over Duna being used to map the planet surface.

  • A small unmanned rover just saw some surface "blueberries"!

  • Duna's surface at dawn.

  • Duna and Ike.

  • A pre-0.21 topographic height map of Duna made with the ISA MapSat plugin.

  • A pre-0.21 color map of Duna.

  • A lander on the northern pole of Duna.

  • Duna at sunrise.

  • A rover at the edge of one of the "sinkholes."

  • A small probe orbiting Duna.

  • Ike partially eclipsing Kerbol. Note the dimmer light and the solar panels not charging.

  • Duna seen from Ike.

  • Duna and Ike as seen from a space telescope.

  • The road to Duna is paved with speedbumps...

  • ...but the journey is worth the effort!

  • A rover on the surface of duna.

Changes KSP1

1.2
  • Added biomes
1.0.5
  • Changed atmosphere characteristics
0.90
  • Added biomes
0.21
  • Art Pass
0.18
  • Minor art pass
0.17
  • Initial Release

Changes KSP2

KSP2 v0.2.0.0
  • Added research locations

Trivia

Egar in orbit of Meander
  • Duna was originally called "Egar" and was in orbit of Meander, the precursor of Jool. It was described as half icy wasteland, half desert. [4]
  • According to former developer NovaSilisko, Duna's appearance was inspired by the theory that ice ages on Mars may have brought the ice caps much closer to its equator. - Meaning that Duna might be in a ice age. [5]
  • Duna's name, which is the Spanish word for dune, may be either a reference to its desert landscape or a reference to the Frank Herbert novel Dune.
  • The low-lying areas near Duna's equator make a shape resembling Europe.
Spoiler: Anomalous features
Kerbal face.jpg
  • On the surface of Duna, there is a large monument carved in the likeness of a Kerbal face, alluding to the infamous "Face of Mars" discovered in the Cydonia Mensae region of Mars during the 1970's.
  • Buried deep under the surface, there is a small camera, similar to the design on the Curiosity rover.
  • One anomalous feature on Duna is a small, pyramid-like hill emitting an SSTV signal. When decrypted, it shows a diagram-like image of three figures standing next to the hill itself, which was originally part of the developer's story but later scrapped.
  • There is a stranded rover on Duna which appears similar to the NASA Spirit and Opportunity rovers.
  • There is one randomly generated green monolith on Duna.
  • It may be possible to reach Duna by year 1, day 2(The next Kerbin Day) by launching immediately with a delta-v of over 2 million m/s.
    • Duna's color map uses some details that are blended in from the old Duna color map (as well as procedural PQSLandControl coloration) however, this color map is from the old version of Duna, before its "revamp" in 0.21. The color map references features which no longer exist on Duna, and is offset by about 180 degrees longitude.

    • References & Notes

    1. ↑ Not a real sea. For real seas, see Kerbin, Laythe, Eve.
    2. ↑ KSP Delta V Planner
    3. ↑ Transfer calculator
    4. ↑ Kerbol System Proposal in the forum by NovaSilisko, Aug 2011
    5. ↑ NovaSilisko's answer in “Duna's ice caps are too big”.
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