Ovantu

(I lied. I need to learn how to actually calculate the density of a hollowed sphere.)
==Technicals==
===Physicals===
The planet has a diameter of 147055.375 kilometers, with the mass being 8.7341 M♃, and the density is 10.069 grams per cubic centimeter. The oblateness is 0.01083264, with the effective temperature being 237.83 kelvin, and the Earth similarity index is 0.422. The rotational period is 8 hours, 19 minutes, and 20.99 seconds, with the axial tilt being 99*13’15.24”, and the ascending node is 239*18’35.28”, additionally, the age is 1.141 million years. The gravity on the equator is 201.68 meters per second, with the gravity on the poles being 209.43 meters per second, and the 1st cosmic value is 122.75 kilometers, additionally, the 2nd cosmic value is 173.59 kilometers per second. 
===Atmospherics===
The planet has an atmospheric pressure that is indeterminate, and the air density is also indeterminate. The effective height is 514.694 kilometers, with the average molar mass being 0.091876, and the relative mass is 0.80246 M♃. The average temperature is 237.83 kelvin, -31.576 Fahrenheit, -35.32 degrees Celsius, with the greenhouse effect being 0 kelvin.
===Orbitals===
The planet has an elliptical type orbit, with its patent being θ Oph, and the orbital period is 597.383 years. The planet has a semimajor axis of 159.421 AU, with the pericentric distance being 146.620 AU, and the eccentricity is 0.080. The inclination is 237*28’57.57”, with the ascending node being 232*9’46.77”, and the argument of pericenter is 23*6’59.08”. The mean anomaly is 224*33’04.95”, with the longitude of pericenter being 255*16’45.85”, and the mean longitude is 479*49’50.80”.
==Store==
===Internals===
The core of this world is made up of molten silicon, nickel, and some small amounts of iron. The core has a mass of 29 Earths, with the magnetic field created by it being 45% stronger than Jupiter’s magnetic field, and the inner or outer core has no real, describable boundary. The core has a “mantle” above it, and superdense layers of hydrogen, helium, and trace amounts of nitrogen and methane sit on top of it. This layer is only 3 Earths in thickness yet makes up 86.7% of the mass, which gives it a density of 0.015 Jupiters per volume of Earth, or 4.767 Earths per Earth volume. This layer of dense gases sits below a thin and significantly less dense layer of more free-bound hydrogen, helium, and some nitrogen, a “crust” of sorts. It is thin enough that flight through it would be more similar to Earth than Jupiter. A strong enough commercial aircraft could go through the top parts of the layer and feel no real effects of the gas giant’s atmospheric turbulence.
===Cloudography===
At the poles, the planet has two massive weather systems, constantly rotating with an average wind speed comparable to Jupiter’s highest. These systems manifest as large and dark cyclones with no outside trails that surround a clam of sorts. A little further to the equator, we have another thick region of the atmosphere, this time a little less cyclonic, dense, and dark. Going further to the equator, we see our first-hemisphere difference. In the northern half, there are two calm and almost non-existent bands, with a stronger band coming right after them, with each having a similar thickness.
In the southern half, there is a darker band, followed by a lighter band, both of which have a noticeable boundary between them, and after the lighter band, we get a moderately thick dark band similar to the polar cyclones. A little further to the equator, the northern hemisphere reaches a similar dark band, but it’s thinner and a little lighter, and beyond it we find a moderate band. In the southern hemisphere, right after the dark band, we find another band of similar thickness but lighter color. In short, the southern hemisphere has thicker and more radical bands than the northern hemisphere. There are two large and very similar cyclones here on each of the poles, with the northern one being slightly stronger.
===Climate===
The climate here is dry and cool. This cool climate is quite comfortable, so long as you forget the seemingly freezing “cool” temperatures that exist constantly throughout the “surface” of the gas giant. The hottest temperatures throughout the year tend to accumulate in a circumpolar ring. These temperatures seemingly do not have an effect on where the highest wind speeds are, which are in the southern hemisphere, with average wind speeds being 50% higher than any found in the northern hemisphere. Add to that, the southern hemisphere also has worse weather, as expected. The average humidity here is low enough that breathing in the air could give you a dry throat, at least in the upper layers of the gas giant. The average weather here consists of dry thunderstorms and hail. Large wind gusts and simple cyclones are also common sights here. Overall, this is a cool, dry, and somewhat stormy climate, typical of any gas giant like it. If you want any sort of temperate temperature, just go to the lit portion of the circumpolar ring, and to boot, the weather here is also more predictable and constant than what is found here on Earth.
==Gallery==
File:Ovantu-002.png
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File:Ovantu-001.png
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File:Ovantu-009.png
File:Ovantu-008.png
==Moons==
The planet has a small array of moons, most of which are easy to colonize. If the parent stars wouldn’t die so early, they could even develop life on them, but, they can not do this with the limited time frame they are given, at best one of them could develop prokaryotes in hot springs in the coasts of whatever bodies of water they have. The reason why 3/4  of the major moons are terras is due to some recent comet bombardment, around ~400 thousand years ago. Most of these moons are not really that interesting on their own, rocks with some wet patches is a good way of describing them.
===Grantuy===
File:Ovantu-011.png
A pretty small moon, this world is a temperate terra. It is swept by a large, barren landscape. The geography here is overwhelmingly land-dominated; around 92% of the surface is occupied by land. The only bodies of water here are small craters from the primordial days, nothing too deep and of a small size, and some of them even feature hotsprings. The most odd part of this moon is the climate. The previously mentioned landscape has moderate humidity and frequently receives small amounts of rain throughout the day. Every square mile of land on this surface receives 0.10 inches of rain every 2 hours, and these little rain spouts last only a few minutes at most. These rain spouts are so frequent that if you were to stand on any one part of the moon, you would see them as a sky army of small clouds with a dark bottom and a fog coming out from underneath them (their rain). It is unknown how this moon’s climate has created this, though it is noted that a possible cause could be that the atmosphere has compounds in certain amounts that elevate rates of precipitation to a sort of sweet spot. Small cyclones are also a common occurrence here, and though they never reach anything more than a tropical storm in strength, they do add to the spotted atmosphere. These cyclones are quite frequent and are common throughout a 365.25-day term. Overall, this moon is a usual dry terra with an exceptional climate, which is sustained by a small number of lakes and the right amounts of certain compounds in the atmosphere. Another fact about this moon is that it has the strongest magnetic field in the moon system, powered by a large and fast spinning core of molten nickel. It is the most likely in the system to develop life.
===Bloscyenen===
File:Ovantu-012.png
This moon is a warm terra and is also the largest of the bunch, having a size 1 ½ times the Earth’s and a mass 5 times the Earth’s. The moon has a thick atmosphere, thick enough that things in the sky are not immediately apparent at first glance. Despite what the parent star projects, the moon does not have a blue atmosphere but a red one, though it could be orange as well, depending on the person. The moon has a slightly higher rate of erosion than the other moons in the system, which explains why, despite its young age, most of the primordial craters have already formed into the landscape. The moon has a roughly even split of land and water and sports a large ocean, with plenty of smaller lakes and seas coming off of it. The moon also sports a large number of islands, around double the amount found on Earth, though most of these islands are located in one of the many coastal marshes. The ocean is bounded by several continents that look to be in an island-type formation, though the sea levels are too low for them to be independent of each other. One of the more notable things here is that the few primordial lakes that have survived so far seem to be staying, and they have a slightly different water makeup compared to the rest of the seas around them, with their makeup being “superfresh heavy water.”. Essentially, these primordial, resistive to erosion craters have a makeup of water that is devoid of most outside ingredients, even more so than the fresh water found on Earth, and it is heavy water, which means it is an oxygen atom with two deuterium(s) attached to it. It is unknown as of yet how this moon has naturally occurring heavy water. The climate here is a little rocky compared to its siblings, with the ratio of “stormy” days to “calm/sunny” days being 5:2. This climate and atmosphere are held to the moon by a surprisingly weak magnetic system, which is 20% weaker than the Earth’s magnetic field. This field comes from a large though slow core, which also means that the future plate tectonics are slow here, around 30% slower than the tectonics found on Earth. Life is not as likely to develop here as on the other moons, having lower chances than even on the desert moon.
===Havienen===
File:Ovantu-013.png
This is an average sized major moon, and it is a temperate desert. This moon has a very thin atmosphere, thin enough that it is barely visible from its own surface, let alone from space. There are hundreds of craters that dot the surface of this moon, creating a geography of primordial dents and flat basins of tanish rock. As a consequence of the un-cleaned bombardment level of craters across its surface, the topography is all out of wack, trying to drive here would be impossible, let alone near one of the basins, which vae large drop offs in unexpected places. The atmosphere here is very thin, but it is not thin enough that it can’t support a small climate of some kind. The climate, limited it is and the term “climate” is being used very loosely here, supports some form of weather. The “weather” here features breezes that you would barely notice, and small, localized, and cloudless snow “storms” where at the very tops of mountains, a little bit of snow can be seen coming from the air directly over the ground. This snow never reaches a thickness more than half a thumb. Besides that, the climate is like an empty warmness, you can only feel the blind temperature and nothing else. This desert moon sports a somewhat active core, a molten ball of nickel and some iron, smaller than the Earth’s core by 1.2%, and it creates a magnetic field 5% stronger than the Earth’s. Of course, this means skyless aurora. Overall, a barren wasteland with little potential to support life, having little to no weather, and having an averageness which makes it forgettable. 
===Iolayo===
File:Ovantu-014.png
This is the last moon in the system, it is a temperate terra that sports large oceans and continents, 6 continents and 4 oceans to be specific. The moon has a moderate climate, similar to the Earth, though it can not support storms stronger than a category 3 hurricane. This climate has an even split of days occupied by storms and days occupied by clear or at least partly cloudy days. The humidity here is average, like that of the Earth’s, and the humidity reaches its peak at the equatorial seas. The moon has a strong potential to support life, like that of the first moon, though it is unknown if the moon has as many ingredients and factors which favor life as much as the first moon does. The magnetic field generated by this moon’s core is comparable to the Earth’s,  and the size of that core is slightly larger than the Earth’s core, and its composition is mostly nickel and some amounts of iron. This moon is not that unique, but it does have the thickest crust in its local area, more than quadruple the thickness of Earth’s crust, which is quite large for a regular terra.
==Entras==
===Moon system===
This planet has a very small moon system, only containing the moons that were listed and described above. There are no other moons around the planet. The explanation for this is that the conditions of the primordial environment that the planet formed in did not favor a large, extensive moon system, only allowing for a small and concentrated one, just like the one we see today. In other words, the material that was not consumed by the formative planet was left in a close-bound ring, and said ring was low in mass, only allowing for a few moons at most, and in this case, it was four major moons.
 	Grantuy 	Bloscyenen 	Havienen 	Iolayo
Image 	
File:Ovantu-011.png	
File:Ovantu-012.png	
File:Ovantu-013.png	
File:Ovantu-014.png
Class 	Temperate terra	Warm terra 	Temperate desert	Temperate terra
Mass 	0.43411 M⨁ 	5.0948 M⨁ 	0.60115 M⨁ 	0.71405 M⨁
Diameter	8550.793 km 	19650.602 km	12075.709 km 	11181.307 km
Orbital 	1.483d 	2.686d 	4.875d 	16.026d
===Star system===
This planet exists in a small, uninteresting star system. It is a binary star system of two higher mass objects. The primary of the two is a blue subgiant, and the secondary is a blue main sequence star. The system has 5 barren, slightly over average sized and massive planets. The planets have a regular distance between each other, and they are all deviant from the plane of the two stars. The system has no asteroid belts and no oort cloud. 
File:Ovantu-015.png
Category:Procedural objects
Category:Objects
Category:Gas giants
Category:Superjupiter
Category:Planets