Chronocide wrote:

Status: Active

Background request!
Better late than never, right?

Background

Image

I hope you like it!

Garalulu wrote:

HYPEEEEEE

Take my star instead of mod >w<

lovely pattern and cool song! maybe I think it's okay

Good luck~

WolfyArmato- wrote:

Hello, From My Queue.

|1|2|3|4|

[furioso divertido]00:04:942 (4942|0) - move to |2|? different pitch with 00:04:555 (4555|0) but need pitch others too and it would break it
00:06:490 (6490|2) - move to |4|? different pitch with 00:06:103 (6103|2) ^
00:11:135 (11135|0) - move to |2|? different pitch with 00:10:748 (10748|0) ^
00:12:684 (12684|2) - move to |4|? different pitch with 00:12:297 (12297|2) ^
00:26:426 (26426|1) - move to |1|? maybe flow better k
00:26:426 - http://puu.sh/qGS7E/fae48202fc.PNG do like this? naah
01:10:458 - add note at |3| it's done intensionally for playability
01:11:232 - add note at |4| and delete 01:11:329 (71329|3) ^
01:11:329 (71329|3) - add note at |3|? cymbal sound here
01:11:329 (71329|3) - add note at |1|? ^
01:11:329 (71329|3) - add note at |3|? ^ wtf
03:43:458 to 03:52:361 - maybe make double on every white line? don't really want to

that's all i can find!
very nice mapping and very good song, i luv it <3
take my star

Protastic101 wrote:

Ay lmaoooo. no kds

Bahhhh

00:01:652 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- This section of the music is great and all, but I do think it could do with A LOT of improvement. I mean, you use 1/6 and 1/4 snaps all the time, and it plays so nicely, plus the patterns are very nice to look at and comfortable to hit. Also, the way that you used the SVs were beautiful because they were easily sightreadable. Plz teech mi hao to SV senpai. Anyways, I really did like the chord layering you did during, because the hardstyle kicks were really powerful and deserved a 3 note chord. My only qualm would have been the quads used when there wasn't a kick, but the sustained sound justified it. Here's a sheep The LNs too fit nicely as they helped the player predict when the next notes were coming which I thought was really nice. Senpai, y u no notice me. Notice me dorian, plis, I beg of u, i am 12 yr/o gamer gurl, pls notice me, i'm so geeky and nerdy becuz i leik to play pokemon go, but im not leik the fake gamer gurlz who only play call ov duty. I feel sick, but I also want to eat some cookies, oh my god, what do I even do with my life urghhhhh. I need something to do besides shitposts in the forums all day. This just makes me sad. I also have homework that I should be doing but am not because I hate myself, you know? Anyways, this wall of text isn't going to be that long, I'm probably going to find a copy pasta in a bit so that I don't have to manually write everything out, brb. Why is the sky blue?
On a clear sunny day, the sky above us looks bright blue. In the evening, the sunset puts on a brilliant show of reds, pinks and oranges. Why is the sky blue? What makes the sunset red? To answer these questions, we must learn about light, and the Earth's atmosphere. The atmosphere is the mixture of gas molecules and other materials surrounding the earth. It is made mostly of the gases nitrogen (78%), and oxygen (21%). Argon gas and water (in the form of vapor, droplets and ice crystals) are the next most common things. There are also small amounts of other gases, plus many small solid particles, like dust, soot and ashes, pollen, and salt from the oceans. The composition of the atmosphere varies, depending on your location, the weather, and many other things. There may be more water in the air after a rainstorm, or near the ocean. Volcanoes can put large amounts of dust particles high into the atmosphere. Pollution can add different gases or dust and soot. The atmosphere is densest (thickest) at the bottom, near the Earth. It gradually thins out as you go higher and higher up. There is no sharp break between the atmosphere and space. Light is a kind of energy that radiates, or travels, in waves. Many different kinds of energy travel in waves. For example, sound is a wave of vibrating air. Light is a wave of vibrating electric and magnetic fields. It is one small part of a larger range of vibrating electromagnetic fields. This range is called the electromagnetic spectrum. Electromagnetic waves travel through space at 299,792 km/sec (186,282 miles/sec). This is called the speed of light. The energy of the radiation depends on its wavelength and frequency. Wavelength is the distance between the tops (crests) of the waves. Frequency is the number of waves that pass by each second. The longer the wavelength of the light, the lower the frequency, and the less energy it contains. Visible light is the part of the electromagnetic spectrum that our eyes can see. Light from the sun or a light bulb may look white, but it is actually a combination of many colors. We can see the different colors of the spectrum by splitting the light with a prism. The spectrum is also visible when you see a rainbow in the sky. The colors blend continuously into one another. At one end of the spectrum are the reds and oranges. These gradually shade into yellow, green, blue, indigo and violet. The colors have different wavelengths, frequencies, and energies. Violet has the shortest wavelength in the visible spectrum. That means it has the highest frequency and energy. Red has the longest wavelength, and lowest frequency and energy. Light travels through space in a straight line as long as nothing disturbs it. As light moves through the atmosphere, it continues to go straight until it bumps into a bit of dust or a gas molecule. Then what happens to the light depends on its wave length and the size of the thing it hits.
Dust particles and water droplets are much larger than the wavelength of visible light. When light hits these large particles, it gets reflected, or bounced off, in different directions. The different colors of light are all reflected by the particle in the same way. The reflected light appears white because it still contains all of the same colors. Gas molecules are smaller than the wavelength of visible light. If light bumps into them, it acts differently. When light hits a gas molecule, some of it may get absorbed. After awhile, the molecule radiates (releases, or gives off) the light in a different direction. The color that is radiated is the same color that was absorbed. The different colors of light are affected differently. All of the colors can be absorbed. But the higher frequencies (blues) are absorbed more often than the lower frequencies (reds). This process is called Rayleigh scattering. (It is named after Lord John Rayleigh, an English physicist, who first described it in the 1870's.) WHY IS THE SKY BLUE
The blue color of the sky is due to Rayleigh scattering. As light moves through the atmosphere, most of the longer wavelengths pass straight through. Little of the red, orange and yellow light is affected by the air. However, much of the shorter wavelength light is absorbed by the gas molecules. The absorbed blue light is then radiated in different directions. It gets scattered all around the sky. Whichever direction you look, some of this scattered blue light reaches you. Since you see the blue light from everywhere overhead, the sky looks blue. As you look closer to the horizon, the sky appears much paler in color. To reach you, the scattered blue light must pass through more air. Some of it gets scattered away again in other directions. Less blue light reaches your eyes. The color of the sky near the horizon appears paler or white. Black sun, white sky? On Earth, the sun appears yellow. If you were out in space, or on the moon, the sun would look white. In space, there is no atmosphere to scatter the sun's light. On Earth, some of the shorter wavelength light (the blues and violets) are removed from the direct rays of the sun by scattering. The remaining colors together appear yellow. Also, out in space, the sky looks dark and black, instead of blue. This is because there is no atmosphere. There is no scattered light to reach your eyes. As the sun begins to set, the light must travel farther through the atmosphere before it gets to you. More of the light is reflected and scattered. As less reaches you directly, the sun appears less bright. The color of the sun itself appears to change, first to orange and then to red. This is because even more of the short wavelength blues and greens are now scattered. Only the longer wavelengths are left in the direct beam that reaches your eyes. The sky around the setting sun may take on many colors. The most spectacular shows occur when the air contains many small particles of dust or water. These particles reflect light in all directions. Then, as some of the light heads towards you, different amounts of the shorter wavelength colors are scattered out. You see the longer wavelengths, and the sky appears red, pink or orange.
Atmosphere timezzz. The atmosphere is the mixture of gases and other materials that surround the Earth in a thin, mostly transparent shell. It is held in place by the Earth's gravity. The main components are nitrogen (78.09%), oxygen (20.95%), argon (0.93%), and carbon dioxide (0.03%). The atmosphere also contains small amounts, or traces, of water (in local concentrations ranging from 0% to 4%), solid particles, neon, helium, methane, krypton, hydrogen, xenon and ozone. The study of the atmosphere is called meteorology. Life on Earth would not be possible without the atmosphere. Obviously, it provides the oxygen we need to breath. But it also serves other important functions. It moderates the planet's temperature, reducing the extremes that occur on airless worlds. For example, temperatures on the moon range from 120 °C (about 250 °F) in the day to -170 °C (about -275 °F) at night. The atmosphere also protects us by absorbing and scattering harmful radiation fromthe sun and space.
Of the total amount of the sun's energy that reaches the Earth, 30% is reflected back into space by clouds and the Earth's surface. The atmosphere absorbs 19%. Only 51% is absorbed by the Earth's surface. We are not normally aware of it but air does have weight. The column of air above us exerts pressure on us. This pressure at sea level is defined as one atmosphere. Other equivalent measurements you may hear used are 1,013 millibars, 760 mm Hg (mercury), 29.92 inches of Hg, or 14.7 pounds/square inch (psi). Atmospheric pressure decreases rapidly with height. Pressure drops by a factor of 10 for every 16 km (10 miles) increase in altitude. This means that the pressure is 1 atmosphere at sea level, but 0.1 atmosphere at 16 km and only 0.01 atmosphere at 32 km.
The density of the lower atmosphere is about 1 kg/cubic meter (1 oz./cubic foot). There are approximately 300 billion billion (3 x 10**20, or a 3 followed by 20 zeros) molecules per cubic inch (16.4 cubic centimeters). At ground level, each molecule is moving at about 1600 km/hr (1000 miles/hr), and collides with other molecules 5 billion times per second. The density of air also decreases rapidly with altitude. At 3 km (2 miles) air density has decreased by 30%. People who normally live closer to sea level experience temporary breathing difficulties when traveling to these altitudes. The highest permanent human settlements are at about 4 km (3 miles). The atmosphere is divided into layers based on temperature, composition and electrical properties. These layers are approximate and the boundaries vary, depending on the seasons and latitude. (The boundaries also depend on which "authority" is defining them.)
LAYERS BASED ON COMPOSITION
Homosphere
· The lowest 100 km (60 miles), including the Troposphere, Stratosphere and Mesosphere.
· Contains 99% of the atmosphere's mass.
· Molecules do not stratify by molecular weight.
· Although small local variations exist, it has a relatively uniform composition, due to continuous mixing, turbulence and eddy diffusion.
· Water is one of two components that is not equally distributed. As water vapor rises, it cools and condenses, returning to earth as rain and snow. The Stratosphere is extremely dry.
· Ozone is another molecule not equally distributed. (Read about the ozone layer in the Stratosphere section below.)
Heterosphere
· Extends above homosphere, including the Thermosphere and Exosphere.
·Stratified (components are separated in layers) based on molecular weight. The heavier molecules, like nitrogen and oxygen, are concentrated in the lowest levels. The lighter ones, helium and hydrogen, predominate higher up.
LAYERS BASED ON ELECTRICAL PROPERTIES
Neutral atmosphere
· Below about 100 km (60 miles)
Ionosphere
· Above about 100 km
· Contains electrically charged particles or ions, created by the absorption of UV (ultraviolet) light.
· The degree of ionization varies with altitude.
· Different layers reflect long and short radio waves. This allows radio signals to be sent around the curved surface of the earth.
· The Aurora Borealis and Aurora Australis (the Northern and Southern Lights) occur in this layer.
· The Magnetosphere is the upper part of the ionosphere, extending out to 64,000 km (40,000 miles.) It protects us from the high energy, electrically charged particles of the solar wind, which are trapped by the Earth's magnetic field.
LAYERS BASED ON TEMPERATURE
Troposphere - Height depends on the seasons and latitude. It extends from ground level up to about 16 km (10 miles) at the equator, and to 9 km (5 miles) at the North and South Poles.
· The prefix "tropo" means change. Changing conditions in the Troposphere result in our weather.
· Temperature decreases with increasing altitude. Warm air rises, then cools and falls back to Earth. This process is called convection, and results in huge movements of air. Winds in this layer are mostly vertical.
· Contains more air molecules than all the other layers combined.
Stratosphere - Extends out to about 50 km (30 miles)
· The air is very thin.
· The prefix "strato" is related to layers, or stratification.
· The bottom of this layer is calm. Jet planes often fly in the lower Stratosphere to avoid bad weather in the Troposphere.
· The upper part of the Stratosphere holds the high winds known as the jet streams. These blow horizontally at speeds up to 480 km/hour (300 miles/hour)
· Contains the "ozone layer" located between 15 - 40 km ( 10 - 25 miles) above the surface. Although the concentration of ozone is at most 12 parts per million (ppm), it is very effective at absorbing the harmful ultraviolet (UV) rays of the sun and protecting life on Earth. Ozone is a molecule made of three oxygen atoms. The oxygen molecule we need to breathe contains two oxygen atoms.
· The temperature is cold, about -55 °C (-67 °F) in the lower part, and increases with increasing altitude. The increase is caused by the absorption of UV radiation by the oxygen and ozone.
· The temperature increase with altitude results in a layering effect. It creates a global "inversion layer", and reduces vertical convection.
Mesosphere - Extends out to about 100 km (65 miles)
· Temperature decreases rapidly with increasing altitude.
Thermosphere - Extends out to about 400 km ( 250 miles)
· Temperature increases rapidly with increasing altitude, due to absorption of extremely short wavelength UV radiation.
· Meteors, or "shooting stars," start to burn up around 110-130 km (70-80 miles) above the earth.
Exosphere -Extends beyond the Thermosphere hundreds of kilometers, gradually fading into interstellar space.
· Density of the air is so low that the normal concept of temperature loses its meaning.
· Molecules often escape into space after colliding with one another.
I CAN READ
Why is the sky blue?
Light is a kind of energy that can travel through space. Light from the sun or a light bulb looks white, but it is really a mixture of many colors. The colors in white light are red, orange, yellow, green, blue and violet. You can see these colors when you look at a rainbow in the sky.
The sky is filled with air. Air is a mixture of tiny gas molecules and small bits of solid stuff, like dust.
As sunlight goes through the air, it bumps into the molecules and dust. When light hits a gas molecule, it may bounce off in a different direction. Some colors of light, like red and orange, pass straight through the air. But most of the blue light bounces off in all directions. In this way, the blue light gets scattered all around the sky.
When you look up, some of this blue light reaches your eyes from all over the sky. Since you see blue light from everywhere overhead, the sky looks blue.
In space, there is no air. Because there is nothing for the light to bounce off, it just goes straight. None of the light gets scattered, and the "sky" looks dark and black.

tl;dr

Stuff

03:28:781 (208781|0,208813|1,208845|2,208877|3,208910|0,208942|1,208974|2,209006|3) - I'm triggered by this blatant abuse of 1/12, it's 1/6 you oppressor. I think. ._. i think it's 1/24 or even 1/32
02:08:619 (128619|0) - This is the same sound as all the other hihats in this section, so remove this note? (or remove the other but move the whistle). it's more intensive from others, that's why 2 notes
02:46:684 - 02:46:942 - 02:47:200 - There are snares here, so consider adding them, but I also don't care since I can just sample them. nope
03:36:103 (216103|3,216361|3) - These two notes aren't the same pitch, so move 03:36:361 (216361|3) to 3. k
03:42:297 (222297|0) - Move this to 3 for pitch relevancy.

Hollas wrote:

ight lets get thhis shhow on the road....

00:01:652 - my personal preference, for the little chimes, i would put very small LNs here nah
00:35:716 - again my preference, for the chime sounds, i'd like to have little small LNs here just to bring a little bit more creativity nah
00:48:103 - i feel like this sv speed up has a very little reaction time to time, try lowering the speed up or the reset time then after the note, go back to regular speed. it's good for me and a lot of testplayers
00:59:331 - here, i hear 3 distorted sounds instead of 2 like shown for the amount of LNs try to add another one but have all 3 shorter. i don't hear it
01:00:490 - for here, if you were going to have doubles for the loud drum, try to be consistent, have as many doubles you want for this sound to spice it up a little k
01:48:103 - try not to have the same roll patterns for that sounds, reverse it going from left to right k
01:50:232 - again "again my preference, for the chime sounds, i'd like to have little small LNs here just to bring a little bit more creativity" nah
02:45:393 - a fade LN should go here with maybe an SV i don't want it
02:52:745 - this LN sound to? try mapping it to the loud 2 sounds with LNs instead if having the 2 doubles, the sound carries out I see no reason, the start of kiai must be 3 notes and in there are 2 notes sounds, 12 12 is boring
02:54:297 - for this try having it has doubles instead of singles for that specific pattern of sounds i don't understand
02:55:071 - the singles for this pattern of sounds is fine again
02:57:393 - another example of having doubles here for that pattern of sounds and again
03:01:264 - stop the doubles here ^
03:03:684 - have the doubles ^
03:06:684 - have the doubles ^
03:09:651 - have the doubles ^
03:12:747 - have the doubles ^
03:29:135 - no 1/4 or 1/6 when the speeds up here? no 1/6 in there
03:30:877 - LN for chimes nope
05:11:326 - LN for chimes nope

DONE!~ GL BRO

MrDurian wrote:

lmao

Alsty- wrote:

hai duren :v
NM as requested. maybe this is will be a short mod , this is already good.
1|2|3|4
00:24:490 (24490|2,24490|0,24684|0,24684|3) - 34 - 12 ? variasi di akhir + pitchnya juga lebih kerasa.
00:57:006 - coba liat https://osu.ppy.sh/ss/6068611 00:57:071 (57071|0,57135|3) - ini susah di pencetnya =3=
01:06:555 (66555|2,66619|1,66684|2) - ctrl+h , kebalikan nya dari yg ini 01:09:393 -
btw kalo ^ di apply 01:09:200 (69200|2,69297|3,69393|2) - jadiin 4|3|4 biar sama jg
01:18:877 (78877|0,78877|1,78974|0,78974|2,79071|1,79071|3) - begh , berat ini , ga coba [12][34][12] , ato [23][14][23] aja?
01:28:555 - hi hat di bagian'' kek gini ga di present ? feel nya kurang lho :/
01:39:974 (99974|1,99974|0,100361|3,100361|2) - ctrl+H , pitchnya , terus 01:40:458 (100458|1,100555|0,100651|2) - jadinya juga bisa dibikin 3|2|1 jadinya ga broken stair , kesian brolken stair sendiri tapi yang next partnya stair alus semua.
02:28:188 - wadoo quadstream , ntaps (y) dah lama ga liat quadstream :3
03:03:587 (183587|2,183587|0,183587|1,183587|3) - ini terlalu over sebenernya , nada nya sama kek 03:02:813 (182813|2,182813|0,182813|3) - maaf , terlihat agak di paksa tbh. kalo bisa di kurangin. terus pertahanin yang 03:06:297 (186297|2,186297|0,186297|1,186297|3) - finish efek bagus.
03:15:877 - bagian ini konsistensinya di liat lagi , kek 03:15:845 (195845|2,195845|0,195845|3) - 03:16:232 (196232|1,196232|0,196232|2) - sama nada nya kek 03:16:619 (196619|0,196619|3) - ini jadiin triple , nah 03:16:490 (196490|2,196490|1,196490|3) - jadiin double
03:17:264 (197264|2,197264|1,197264|3,197393|0,197393|1) - sama ^ , di balik valuenya
04:06:877 - https://osu.ppy.sh/ss/6068895
04:27:877 (267877|0,267877|2,267974|1,267974|3) - 2|3 - 1|4 @@ ato kek 04:40:168 - masih enak di pencetnya :/
05:12:684 (312684|0,312781|3) - ctrl+h 05:12:490 (312490|0,312684|0) - beda ama yg lain nya , biar lebih rapih aja.
sorry no offense , diriku kadang hanya ga suka sama pattern yang agak susah di pencetnya. :3
makasih dah request , GL duren :3

I'M POLISH, NOT INDONESIAN XDDDDDDDDDDDDDDDDDDDDDD

Alsty- wrote:

hiiiiii :v
NM as requested. maybe this is will be a short mod , this is already good.
1|2|3|4

mod

00:24:490 (24490|2,24490|0,24684|0,24684|3) - 34 - 12 ? variation in the end + pitch. k
00:57:006 - look this https://osu.ppy.sh/ss/6068611 00:57:071 (57071|0,57135|3) - a bit complicate =3= nah, like I had something like that before and now I wanna trill
01:06:555 (66555|2,66619|1,66684|2) - ctrl+h , the reverse of 01:09:393 - okay
btw ^ if above applied 01:09:200 (69200|2,69297|3,69393|2) - make em 4|3|4 k
01:18:877 (78877|0,78877|1,78974|0,78974|2,79071|1,79071|3) - too heavy ? try [12][34][12] or [23][14][23] ? It plays really good, I'll leave it as it is
01:28:555 - hi hat in these part ? on every hihat on this part, i dont get all the feel when i testplay it In kiai I didn't mapped them intentionaly
01:39:974 (99974|1,99974|0,100361|3,100361|2) - ctrl+H , pitch , then 01:40:458 (100458|1,100555|0,100651|2) - thse part can be arrange 3|2|1 i see this part get broken stairs , make it same with the next pattern.. I did it in other way, but thanks
02:28:188 - nice quadstream. :3 thanks ;3
03:03:587 (183587|2,183587|0,183587|1,183587|3) - itbh this too.. , the sound is same with 03:02:813 (182813|2,182813|0,182813|3) - sorrt , looks like a bit forced too. if can , reduce abit of them. but this is a great fnish effect 03:06:297 (186297|2,186297|0,186297|1,186297|3) - don't understand
03:15:877 - check again the consistency on this part, like 03:15:845 (195845|2,195845|0,195845|3) - 03:16:232 (196232|1,196232|0,196232|2) - the sound is same with 03:16:619 (196619|0,196619|3) - ithis is shld be triple , nah 03:16:490 (196490|2,196490|1,196490|3) - make this double
03:17:264 (197264|2,197264|1,197264|3,197393|0,197393|1) - same ^ they were done intentionally, because I don't wanna >4 1/3 jacks
04:06:877 - https://osu.ppy.sh/ss/6068895 I don't want to make one side stream
04:27:877 (267877|0,267877|2,267974|1,267974|3) - 2|3 - 1|4 @@ or like 04:40:168 - it's easy to read and execute
05:12:684 (312684|0,312781|3) - ctrl+h 05:12:490 (312490|0,312684|0) - feels like different with other. okay

thank you for request. GL :3

EYA- wrote:

Hi~Im from Pelmeshki modding queue, wanna buy some weird patterns?
1 | 2 | 3 | 4

hard to read name of difficult

00:01:652 - place notes like this https://puu.sh/rfyVM/f05c60df89.png no, I like my pitch revelancy more

00:06:297 - https://puu.sh/rfz3Z/24765e2758.png ^

00:09:393 - https://puu.sh/rfz4K/4e6d5ab356.png ^

00:37:071 (37071|1,37168|2,37264|3,37264|0,37458|2,37555|3,37651|1,37651|0) - what i can see here looks a bit weird try it https://puu.sh/rfzdD/bbb5cbea11.png k

00:39:006 (39006|2) - to col 2 k

00:40:264 (40264|3,40361|2) - reverse 3-->4 4<--3 no, let's give it some variety

00:40:555 (40555|3,40748|2) - ^ ^

00:44:039 (44039|3) - to col 3 k

00:49:200 (49200|0) - https://puu.sh/rfzmu/4a6cca2cea.png no

00:52:168 - https://puu.sh/rfzoq/8fd5aaf737.png ^

00:55:845 (55845|3,55942|3) - oh myyy... thats to close| move to 3 ^, because too big jack

00:58:361 (58361|1,58426|0,58490|2,58555|3,58748|2) - https://puu.sh/rfzsb/4d1b76c7f9.png no

01:21:781 - https://puu.sh/rfzxF/d415cb5f1a.png no

01:28:361 (88361|1) - to col 1 red

01:31:264 (91264|3,91361|3) - too close its playing uncomfortable i don't think so

03:55:458 - 04:06:684 - overmapped part it isn't overmapped bby

So ur map have a lot of ovemapped moments, and it can be a reason to dq it, but at first look ur map looked awesome it wasnt boring during i mod it.

_RamiWins_ wrote:

Hey just finished your mod ...

armonia fortissima

00:46:748 (46748|1) - to 00:46:893 (46893|0) - try smth. like this https://osu.ppy.sh/ss/6167574 nah
00:49:458 (49458|0) - try adding a LN on column 2 and 3 end at 00:49:587 (49587|2) - 1/6 snap
(maybe delete the note in column 0?) nope
00:51:135 (51135|2) - make this a double just for consistency it was done for playability
00:55:845 (55845|3) - feels weird to play try smth like this https://osu.ppy.sh/ss/6167559 don't really like it
01:10:458 (70458|2) - to 01:10:458 (70458|2) - that change in jump thrills is really weid would suggest making it like this https://osu.ppy.sh/ss/6167549 kay
02:27:974 (147974|0) - to 02:34:168 (154168|0) - the quads make this part very uncomfortable try replacing them similar to this: https://osu.ppy.sh/ss/6167688 everytime they show up it fits more to the tone as well nah
02:37:264 (157264|3) - to 02:37:910 (157910|2) - I think this sectoin of the burst is way to
confusing try this: https://osu.ppy.sh/ss/6167730 done this in other way inspired by yours
03:54:135 (234135|2) - not sure but I think ther should be a note it is

sry for the pretty short mod but tbh. this map is really good and I hope this gets ranked soon... GL still

Adiopulse wrote:

Adiopulse's Signature Tyler1 Skip

[box=melon]01:39:974 note any col u r right, I forgot about these
01:40:168 ^

01:50:039 add lns for the wubs no

02:11:716 i think this drum section should just be doubles to here 02:14:813 - no, notice, what sounds i mapped with doubles
02:47:329 to 02:51:976 ^

03:24:490 these singles should be jacks, and go with the doubles I made this, to create parts that are later easier/box]

Nivrad00 wrote:

BN check

General

I think the offset is a little late. I suggest using 1642 (-10)... does that sound right to you? Remember to resnap green lines and preview points afterward It doesnt sound right to me, it sounds a bit off, so I'll leave old offset (and I took it from Alumetorz map, so it have to be good)

Add BMS to the source pls

Hitsounding

Fantastic hitsounding Protastic

01:03:587 - finish maybe?
01:12:877 - missing clap
01:43:845 - this is a silly thing to point out because it's not even audible... but why is there a whistle fail by prota :^)
02:34:168 - missing sanre
02:34:555 - i don't think there should be a crunch kick here
02:46:813 - missing finish
05:08:232 - missing finish

I encourage you to look over the hitsounds before my recheck, it's better to have two pairs of eyes checked :3

Mapping

00:53:426 - should this be a double for the bass drum? right
02:49:135 (169135|2,169135|1) - why not move this to the third and fourth lanes? that way it's consistent with the "repeated chord" pattern I'm mapping doubles for these weird squishylike sounds and I try to express their pitch, that's why they are like that, but thanks for that, I found something to change : D
02:51:974 - I'm a little concerned about this part. This SV seems pretty misleading. The double-LNs look longer than they should because of the high speeds, and there's no note on the beat at 02:52:361 - so the rhythm can get confused. I think the best solution is to add a note or two at 02:52:361 - to represent the growly bass oki
02:36:877 (156877|0,156877|1,156942|2,156942|3,157006|0,157006|1,157071|2,157071|3) - this is a pretty strong pattern for a light sound. It might be better to use singles. it would also help differentiate this sound from the bass drum! oki x2
03:27:974 (207974|1,207974|0,208039|3,208039|2,208103|1,208103|0,208168|2,208168|3) - same
03:26:813 - i'm a little confused about the chord sizes here. it seems like 03:27:200 - should be a single true, and 03:27:458 - should be a triple actually there's sound for 4 notes, listen closely, w/o hitsounds (and I need to add finish)
03:16:232 - it might just be me, but this part feels really harsh compared to everything else. Maybe you could lower the density in some way? You could replace some quads with triples or replace some triples with doubles ;n; b-but quads ;w;w;w; changed, hope it's good ;w;

Mapping, background, and hitsounds all look great. Good work everyone ^^

Awaiting your response

Nivrad00 wrote:

Rechecking hitsounds

00:48:297 - I dont think this note should be here? in this part I want to put notes only on the instrument and the thing u noted is hihat
you should really add a clap hitsound every time there's a finish hitsound. for example, 00:48:103 - 00:51:200 - 00:54:297 - 00:57:393 - 01:00:490 - etc (there's a lot of them). you can clearly hear the kick on all of them. kay
00:59:619 ]- 01:48:297 - 01:49:716 (109716|2,109781|1,109942|2) - these aren't missing claps, because claps are on 1/8, I was mapping 1/6 sounds (the instrument)- 04:51:974 - 05:09:587 - 05:11:006 (311006|2,311071|0,311232|2) -as before- missing claps
01:43:845 - 01:45:393 - 04:15:587 - missing finishes
00:49:651 - 02:44:103 - extra claps
04:17:135 - missing both finish and clap

I would appreciate if you gave your new hitsounds another quick check before I rebubbled kay