SCIENCE&ARTWORK | PLANET NIRANTO | PART 2

nmɽaŋto

Last post I did a quick sweep over my friend's planet, Niranto, now, we are going to take a look on how I did help him build his conscript for a conlang.

When he first showed me his conscript, I was told he only had the symbols and a few words, but not actually any standardized romanization or sounds for them, recurring to actually using Dovah for the words, and his symbols for the script.

Here is original material he sent me:

Symbols read in order: Dratyr, drenuryr, amackbal, lunmyen, argmotey, dreduryr, omalimack, tarundiun, trockorenis, lapyr, trefinuda, lacbalu, myurdegon, amadilac, uderyon, traccrat

These symbols were initially carved in clay using fingernails, which for most of them, makes sense, that's until we notice some first incongruences...

Green = doable, Yellow = somewhat doable, Red = nope

I have recently processed a block of clay with which I made a Cthulhu statuette, so I used my nails and clay to actually test the feasibility of the symbols created and pointed out we may actually have to re-write the system entirely.

Ph'nglui mglw'nafh Cthulhu R'lyeh wgah'nagl fhtagn

First things first, we defined what are the parts of the symbols called, that would help us structure it better.

We defined that each symbol would be formed by 3 major parts, the lateral Trajulo, the superior Trajulo, and the Surtana.

The Trajulos frame the Surtanas like so:

Dratyr symbol parts

The reading of the symbol would be in U shape, like so:

Reading direction and elements a through e noted

I would use the Dratyr symbol as a model for the others, I also suggested the use of plant bark, such as junciform or bamboo-ish plant as a full time tool or auxiliary tool for more acute curves.

Testing the mechanics of the symbols for a couple words

And once we assigned a syllable or sound to each part variant, we created this table:

Most of words start with a lateral Trajulo, and a few have to start with a Surtana - bellow, some important words, the names of the celestial bodies and the language itself.

included IPA notation and romanization

Differently from Hoku (which is my conlang I'm yet to present to you), and Japanese/Chinese, the symbols in stand more for the sounds they represent than it's actual meaning - which I believe would be long lost in the past already, so I would say that even know I could learn to read this, I could never really guess what's written on it, not without a previously built dictionary in my head.

And here is the phonetic inventory:

Consonant inventory

↓Manner/Place→	Bilabial	Labiodental	Alveolar	Palato-alveolar	Retroflex	Palatal	Velar	Glottal
Nasal	m		n				ŋ
Stop	p		t d	c			k ɡ
Affricate
Fricative			s			ʝ
Approximant
Tap Trill			r		ɽ
Lateral approximant			l

Vowel inventory

	Front	Central	Back
High	i:		u
High-mid			o
Low-mid	e
Near-low	a

Unfortunately, as it is a work in progress I cannot really make an in-depth review of Kygenun language until more is developed about it by my friend Ozeias - so that's the end, so far...

- M.O. Valent, 19/08/2020

PLANETARY MODEL | PART 7 | FIRST STEPS INTO CLOUDS AND WEATHER SYSTEMS

WHAT'S THE WEATHER FORECAST?

...YES >:)

True-color composite of Earth

Credits: NASA

One of the first things we notice while looking back at our blue planet (after it's blueness) is it's cloud cover, of course we would, it covers up to 60% of Earth's surface, cloud systems are a major part of Earth's weather, and it's a shame that we - as worldbuilders, couldn't describe it's beauty properly for years, at least, not that I'm aware of...

If you like to plan every possible detail about your world - like me, then you would be familiar with the >sigh< sensation of having to pick a blue-marble transparent cloud cover like one of these:

I couldn't find further references to designing cloud systems for your planet, for years, I had to pick some of those, I generate clouds procedurally, which actually been quite of headache to piece together, because it looks so artificial.

See, cloud systems are very particular when we look at our own Earth, they are structures within structures, within structures, going down all the way to those 'simple' lone clouds in a sunny day...

lone cloud I found on Reddit

Two days ago, I was working on planet Niranto, when I finished the world map and vegetation I was like

 "Fine, what now?... Clouds?"

Instead of going forward and making a cloudless render, I decided I would investigate what's behind of it, or at least, try finding correlations between clouds and what I already had.

BASIC IDEA

You see, clouds on Earth are made of water vapor that forms little droplets when they meet with tiny dust particles in the air, Mie scattering makes them look white the same way fog does look white.

Clouds can be made of other substances too, on Venus they're made of Vitriol (sulfuric acid), and on Mars, they're made of carbon dioxide, on the gas giants, they're made of ammonia and methane vapor, on Titan, they're made of methane, ethane and other hydrocarbons.

Every planet has it's cloud composition and processes but, the formations are defined by the same mechanisms, temperature and wind pattern.

Too hot and the substance becomes too disperse to form a cloud, too cold and it's probably already frozen in the surface.

Let's take a look at Earth's cloud formations for an instant:

Earth during solar eclipse

Credits: CIMSS

You may have noticed that despite the clouds are moving, they do move in certain patterns, along certain gyres and streams, we can see this by looking at other images of the same region at different times, the next image was taken 2 years after the first.

Negative infrared image of Earth

credits unknown

There is this site that allows you to check different informative maps of Earth, from humidity to ocean wave directions.

Here an ocean currents map map:

Slow currents shown in dark blue, and fast currents shown in red

And then the wind pattern near the surface:

Fast winds shown in green, while slow winds shown in blue

We also see surface temperature seems to be more connected to elevation than wind direction, due to the amount of air around that can hold onto heat:

Hot shown as red and cold as purple/blue

Also relative surface humidity is low where the landmasses are both hot and on high elevations:

High surface humidity shown as cyan, while low is shown as orange

Precipitable water will occur where isn't too cold for snow, but also not too dry:

Looking at cloud map, we see that clouds forms in 2 occasions, when the currents clump together, when the humidity is relatively high.

Dark blue is low/no cloud density, while white is high cloud density

Here is a gif showing that the cloud formations form around clumping winds:

This one shows surface humidity, wind direction and clouds:

Based of that, we now have the basic knowledge to start describing at least - the large cloud formations of our planet...

MAPPING CLOUD SYSTEMS

Let's recap what we must consider:

1. Wind direction.
2. Where the wind fluxes clump together.
3. Relative humidity in the atmosphere and surface.

STEP 1: MAP OCEANIC CURRENTS

Let's first start with a base map of oceanic currents:

Planet Niranto is mostly ocean, which means that most of the winds a and currents will be purely dictated by the Coriolis effect

Then, let's further develop this map, trying to evenly space the current lines where it is possible:

Notice how there is places where the winds cram together to fit there, we will use that cramming to determine where evaporation is occurring more.

STEP 2: MAP OCEANIC EVAPORATION

Blur the image and increase contrast to separate the isles of major density.

STEP 3: MAP PRESSURE REGIONS

Let's take a look at Pressure Map of the Earth:

Notice that high pressure regions occur where the Ferrel and Hadley cells descend, near the tropics, and low pressure regions, in the Intertropical Convergence Zone and the polar fronts, where the winds ascend in the atmosphere.

Landmasses are by default slightly low pressure regions because of elevation, high pressure pockets lag behind orographic barriers (mountain ranges and high elevations).

Following these guidelines I did this map:

High Pressure and Low Pressure systems, change over the course of the year, as temperature gradients change with seasons, so one cloud map fits only one instant of this cyclical process.

High pressure zones push air, while low pressure zones pull air, and also using the Coriolis motion, and the orographic barriers, we can establish the true direction of winds on this planet:

 For this particular post, I will work with a simple wind map like this

STEP 4: MAP THE CLOUDS

Now with this wind map and the evaporation map, we will mark where clouds form, and in which direction they are carried by the wind:

No wind considered

Once you have sprayed the base sources of clouds for that particular configuration, drag the clouds with the wind:

We see the contradicting winds create gyres and single winds drag the clouds around, this ma still have some minor distortion issues we will solve later

Using sprinkled brushes for both painting and dragging the clouds along the lines, I corrected the polar gyres by using polar distortion function in GIMP and then reverting back to a cylindrical projection, for this reason, polar regions usually lose a lot of quality, unless rework is done in the cylindrical final - which I did not re-work

And then, for a humidity touch, I added a polar haze to the map:

Animating such a cloud map would require +30min per frame, even if you know what are you doing right away

FINAL RESULT

Let's compare my first guess on cloud mapping with this new one we learned to make:

 This one I made using the argument of where cold and warm winds meet each other

This one went through all this process of thinking and work

Notice how our well-thought work looks way more natural than the other - of course, it still an utterly simplified model, compared to Earth's complex weather patterns, and also considering Niranto is larger than Earth, those clouds are larger than entire continents, this cloud map would still need some more work to really appeal to a photo-realistic result, but it would be easier to use that result as a base for a new texture than start out of thin air.


That's all I will go through for today, and hopefully you all learned something very useful for your worldbuilding projects - some other day, I will get deeper into this matter and discuss weather in depth.

- M.O. Valent, 19/08/2020

SCIENCE&ARTWORK | PLANET NIRANTO | PART 1

IT ALL STARTED WITH A WAR GAME...

Last week, I was getting without ideas for writing the lore of an alien people - the Hoku, so, to represent the past 200 years of great battles and conquests of those people, I invited, my cousin and his friends to play a game - we would basically play War, in the worldmap of Hokushoku.

And well, once I started naming places, I found out that my cousin's friend, Ozeias, was also into worldbuilding and were getting started into conlanging too - so, I offered my help, and in turn he would let me write about the process.

We chatted all evening yesterday (as I started writing this post), and here is some of what we talked about:

So, in summary, among other stuff we discussed, we defined that the planet, which he called Niranto, would be an Oceanic Super-Earth, with two large and close moons, the moons would cause immense tides, orbiting a close-binary system - the exact data on it would be at my criteria, as long as it does fit the given description.

We one of the first things that I've showed him was the proper size relation of the planet and it's moons, to the Earth and the Moon.

We would still talk a lot while I calculated his parameters and corrected myself over dozens of tries to fit certain aspects, like moon periods.

I've sent several tables, and updated them as we discussed further, and we also accorded to make some visuals so he could properly visualize it

THE STARS

The members of the binary system are Kratyr and Amakbal:

Kratyr

G1V

1,05 Msol

1,14 Lsol

1,04 Rsol

Angular size in the sky 0,46°

Amakbal

M0V

0,45 Msol

0,12 Lsol

0,55 Rsol

Angular size in the sky 0,25°

The Sun compared to the two stars of the system

The two stars would be separated for 0,124 AU, having an orbital period of 13,13 Earth days, and as seem from Niranto, would have an average angular separation of ~5,9°.

To calculate the angular size of your star, or the angular separation of your binary stars as seen from your planet, just use this equation:

ang = (size * 57,29) / distance

In this case, use both size and distance in kilometers, the diameter of your star, times 57,29, then divided by the orbital distance of your planet in AU times 150 million km.

THE PLANET

In this case, using our calculators, I adjusted the planet distance and atmosphere so the planet would have an average temperature to about 17,6°C.

Niranto

PHYSICS

Mass: 5,10 Me

Radius: 1,76 Re (22.425,92 km in diameter)

Density: 5,15 g/cm³

Gravity: 16,17m/s²

Orbital distance: 1,2AU

Orbital period: 393d

Rotational period: 1d 3h (27h)

ATMOSPHERE

Mass: 4,6 atmospheric masses

Composition: 72% N², 27% O², 0,08% CO², 0,30% H²O, 0,00018% CH⁴, 0,70% Argon and other gases.

Greenhouse potential: 1,37x

Average surface temperature: 17,62°C

Pressure at sealevel: 1,49 atm

Air density: 1,81 kg/m³

Scale height: 4,34 km

Niranto's World Maps

The larger continent on the right-side is roughly the size of Russia, while the continent left to it is little smaller than Australia

Oceanic Currents map

Oceanic migration routes, departing from the tiny island continent on the center of the image

THE MOONS

Clary

Mass: 0,04 Me

Diameter: 5.096,8 km

Density: 3,44 g/cm³

Gravity: 2,46 m/s²

Orbital distance: 229.356 km

Orbital period: 5d 14h

Visual Magnitude when full: -12,91

Joan

Mass: 0,026 Me

Diameter: 4.459,7 km

Density: 3,34 g/cm³

Gravity: 2,08 m/s²

Orbital distance: 445.970 km

Orbital period: 15d 4h

Visual Magnitude when full: -11,17

And using Artifexian's tide calculator, I placed the moons (both tidally locked btw) in such a way that the standard tides would be of ~15,8m tall.

The angular sizes of the moons, Clary and Joan, are 1,34° and 0,59 °, respectively, compared to the Moon's ~0,52°

END RESULT

This is how the planet and it's moons were rendered as the final result:

Both planets and their moons, side-to-side for scale

Besides, improving my own skills using Excel, and the calculator itself, I also learned key-steps into making cloud formations, which as a thing I wasn't able to do for a long time, nor properly find it on the internet - I decided that's a post I will make soon, especially for you guys that are kinda tired of relying on NASA's blue marble cloud textures - like me.

NEXT POST I WILL BE REVISING HIS CONSCRIPT, stay tuned...

- M.O. Valent, 14/08/2020