README.md

---
license: apache-2.0
language:
- en
tags:
- MOE
- Qwen 2.5 MOE
- Mixture of Experts
- 6X1.5B
- deepseek
- reasoning
- thinking
- creative
- 128k context
- general usage
- problem solving
- brainstorming
- solve riddles
- story generation
- plot generation
- storytelling
- fiction story
- story
- writing
- fiction
- Qwen 2.5
- mergekit
pipeline_tag: text-generation
---

<H2>Qwen2.5-MOE-6x1.5B-DeepSeek-Reasoning-e32-gguf</H2>

This is a highly experimental Qwen 2.5 MOE (Mixture of Experts) model comprised of SIX Qwen 1.5B models.

It includes the following models:

Captain/Controller (and "shared expert" at .01):

- DeepSeek-R1-Distill-Qwen-1.5B-uncensored

Main Experts:

  - DeepSeek-R1-ReDistill-Qwen-1.5B-v1.1
  - Qwen2.5-DeepScaleR-1.5B-Preview
  - QwQ-R1-Distill-1.5B-CoT
  - DeepSeek-R1-ReDistill-Qwen-1.5B-v1.0
  - DeepSeek-R1-Distill-Qwen-1.5B-uncensored
  - Qwen2.5-1.5B-Instruct

Context: 128k.

You need to use the "Jinja Template" encoded in the GGUF to use this model. You might be able to use Llama 3, and/or Chatml templates
if your AI/LLM app can not access the "Jinja Template".

In Lmstudio the "Jinja Template" should load by default.

In other apps - use the Deepseek Tokenizer.

Sometimes this model will output Chinese Characters/Symbols - regen to clear.

Sometimes it will work great, other times it will give "so/so" answers and then sometimes it will bat it out of the park, and past the "state line."

And sometimes it will output well... less than acceptable.

It is all over the map.

Also, this model has 4/6 experts activated.

You may want to set 6/6 experts for best results.

This model is also mastered in Float 32, which helped overall model generation and addressed some model issues.

Temp of .4 to .8 is suggested, however it will still operate at much higher temps like 1.8, 2.6 etc.

---

Example Generation:

Q8_0 Quant, Temp 1.5, rep pen 1.1, topp: .95, minp: .05, topk: 40

---

<B>Explain ways to use the "night" time cooling of radiant energy into space to reduce global temperatures.</B>

[[[Thoughts Start]]]

Alright, so I need to figure out a way to reduce global temperatures by utilizing the "night" time cooling of radiant energy. Hmm, that's confusing because the term "night time" doesn't quite make sense on its own.

perhaps it means the transition from day to night or from light to dark? That makes sense because in the context, maybe we're talking about the difference between daytime and nighttime lighting, like day and light days vs light days. Maybe that's how they mean 'night'.

If I assume that it's referring to the time when light turns into darkness (like a sunset), which is similar to nighttime as well, then I can think about why temperature reduces around dark hours or night.

In that case, perhaps the idea would be about cooling of energy during the dark hours. So during daytime and during dark times, the energy radiated from objects enters the atmosphere as heat, while in the day time (or dark time?), maybe we are saying when it is just going to something like an earlier state.

Wait no, that seems unclear.

Alternatively, perhaps thinking about how energy or energy is being transferred for cooling, as well as some sort of radiation at the time. Maybe that's a way.

Alternatively, perhaps I'm getting stuck here because in the context, I don't understand what it's all referring to, and why the term 'night' so much isn't sense. So maybe in the context, they must refer to some different kind.

Maybe if this is taken as saying, when time turns from dark hours or light days to day into or vice versa.

Hmm.

Alternatively, perhaps we can think about energy radiated via surface radiation from a body, for example.

Wait that seems another idea. Hmm.

Perhaps the idea of reducing global temperature comes from how we transfer radiant energy between bodies and their surroundings as heat when they have a balance of radiation energy, in the same period or so, but as the time increases.

Wait maybe this is too long, I'm going around circles now.

Alternatively, perhaps to reduce the overall temperatures, using radiative energy through surfaces as heat is efficient because if we can control that, then it reduces the energy for the whole of our planets.

Perhaps something like when during night (dark hours) and during day (light) so have in which they are balancing different radiation of surface to achieve equilibrium or similar to each other. So maybe we can take that approach by calculating how much energy is being radiated as heat.

Alternatively, perhaps the idea is considering the way we move the energies from the air bodies to the atmosphere as Heat energy from the body objects into the atmosphere via radiation. Perhaps at the night time, and then during day, it's different because in their radiations are dissimilar.

But when that the concept makes sense is? Hmm, perhaps not too helpful for me.

[[[Thoughts End]]]

OUTPUT:

To reduce global temperatures using &quot;night&quot; time cooling of
radiant energy from space to achieve an equilibrium where the energy
transitions between body and surroundings can be balanced or
maintained through surface radiative transfers as Heat Energy.</p>
<p style="border: none; padding: 0cm">Alternatively, think about
energy balance during dark periods compared with light times:</p>
<p style="border: none; padding: 0cm">At day (light) and night
(dark), if there are differences in the amount of radiated energy
(H), when their differences vary over time; by considering such
energy dissipation (at each instant).</p>
<p style="border: none; padding: 0cm">If these variables differ in H
from their previous rates, at equilibrium, it's acceptable to allow
H1 = -H2 = -H3 = -H4, balancing for heat transfer through surface
transfers as Heat Energy. It is better for the atmosphere.</p>
<p style="border: none; padding: 0cm">Therefore, during dark periods
and light times (or days) and we consider when we have similar
radiated energy of H:</p>
<p style="border: none; padding: 0cm">At day versus at night; so, in
other way: The time when energies from surfaces into the atmosphere
via Heat Energy are balanced according to that, or we can find energy
H1 = -H2 etc., as needed for maintaining the equilibrium between Day
and Night (or Light and Dark) periods.</p>
<p style="border: none; padding: 0cm">But maybe a different approach
is useful:</p>
<p style="border: none; padding: 0cm">Maybe during dark times, when
an object gives off energy via radiative from its surface, to Earth's
atmosphere as heat, through the surface.</p>
<p style="border: none; padding: 0cm">The idea that when the net
amount of H in terms of the rates is constant between day (H1= -H2)
and night( H3 = H4), then we can arrange so.</p>
<p style="border: none; padding: 0cm">So if we have energies for day
being positive or negative compared with night, during days at night
as heat transfer via surface; hence to get an equilibrium at net.</p>
<p style="border: none; padding: 0cm">This allows us the energy in
such way from body surfaces (and Earth's) as Heat Energy, when net
radiated on a surface is equilibrated so that we can maintain global
temperature equilibrium through H1 and H2 of day ornight rates.</p>
<p style="border: none; padding: 0cm">Hmm, this makes sense. Maybe by
adjusting net rate of radiations during dark and night periods
accordingly for an equilibrium between, it reduces the energy
transfers as heat, leading us to balance or achieve the global
temperature. Thus, with the surface-based energy (Heat via Radiative)
in such a manner can be used to reduce global temperatures.</p>
<p style="border: none; padding: 0cm">But this seems correct? So I
think that by utilizing surface radiative cooling from objects to
Earth at night and during day time rates equating so that net H1 =
-H2 as during day; but we must look for an equilibrium between them.
It means balancing the rate of energy as heat via radiation through
surfaces.</p>
<p style="border: none; padding: 0cm">Alternatively, perhaps another
way is better:</p>
<p style="border: none; padding: 0cm">During dark times and during
days, when net radiated on surfaces are negative or positive
accordingly according to that, such a manner.</p>
<p style="border: none; padding: 0cm">At day and night (H1= H2; so in
H) from object's surface.</p>
<p style="border: none; padding: 0cm">So in the situation of being an
equilibrium where rates are equal via surface:</p>
<p style="border: none; padding: 0cm">If we have a ratio for day or
at night with rates: let H = -h.</p>
<p style="border: none; padding: 0cm">At dark times as h, so net heat
would be (-h). Wait confusing perhaps more simply to say during each
and each time when object is providing heat cooling the Earth's
surface (if during dark), it may need a higher temperature.</p>
<p style="border: none; padding: 0cm">So how does that transfer:</p>
<p style="border: none; padding: 0cm">Thus, maybe during light and
day: Heat can be obtained through radiation of energies from objects
into heat energy via surfaces.</p>
<p style="border: none; padding: 0cm">It would help to think about
how during dark periods, objects emit more radiative on earth than in
day periods. Maybe this way reducing temperatures accordingly for the
equilibrium.</p>
<p style="border: none; padding: 0cm">Alternatively, perhaps the idea
is better used as a form that energy's transfered from objects into
heat via surface in both light times and night (time) respectively as
such an equilibrium to maintain temperature balance: the net effect
can be used to reduce global temperatures.</p>
<p style="border: none; padding: 0cm">Hmm maybe yes.</p>
<p style="border: none; padding: 0cm">To reduce global temperatures
by using &quot;night&quot; time cooling of radiant energy from space,
we aim for balancing radiative transfers during day with dark
periods. When H is the energy transferred in surface cooling, at each
period (light and dark times), their net effects balance through H1 =
-H2. This ensures a steady temperature distribution without excessive
heat flux, allowing us to stabilize global average temperatures
effectively.</p>
<p style="border: none; padding: 0cm">Thus, we can consider how this
energy transfering in surfaces impacts the overall equilibrium of
global warming rates; ensuring that both light periods (H) and dark
periods (H), have balanced effects through their H net transfers—
so we can manage the entire radiation without excess heat loss or
gain. Therefore, by utilizing this balance in surface cooling via
radiant energy at times, night time and day periods accordingly
balancing each other per period, we achieve a stable global
temperature equilibrium.</p>
<p style="border: none; padding: 0cm">Therefore, using surface
heating from objects during both light periods and dark periods
allows us to maintain energy flux without excessive dissipation (in
the Earth), while stabilizing global warming. So the answer is:</p>
<p style="border: none; padding: 0cm">**We can reduce global
temperatures by ensuring that in daylight periods and at dark time
period of radiant energy transfer between surfaces balanced
appropriately, thus managing energy flux to prevent heat fluctuations
and thereby stabilize overall temperature levels.</p>
<p style="border: none; padding: 0cm">To explain ways to use &quot;night&quot;
cooling of radiant energy from space for reducing global
temperatures.</p>
<ol>
	<li><p style="border: none; padding: 0cm"><span style="display: inline-block; border: none; padding: 0cm"><strong>Understanding
	the terms:</span></strong><br/>
The term &quot;night&quot; likely
	refers to when light turns dark or vice versa in time. For example,
	the transition from light to dark or the transition between day into
	night is important because it helps in understanding the changes in
	radiation as the time progresses. This period can help us observe
	the effect of radiation transfers during different stages.</p></li>
	<li><p style="border: none; padding: 0cm"><span style="display: inline-block; border: none; padding: 0cm"><strong>Analyzing
	the idea behind reduction of global temperatures:</span></strong><br/>
Global
	temperatures can be reduced through managing radiant energy transfer
	across surface. Here, considering that during day and at night are
	separated by their radiative energies from objects, and they
	interact in a certain way or ratio.</p></li>
	<li><p style="border: none; padding: 0cm"><span style="display: inline-block; border: none; padding: 0cm"><strong>Key
	point for understanding:</span></strong><br/>
If we manage the
	radiant transfers in surfaces of radiation from objects to Earth,
	balancing these during days periods with at night periods will help
	in achieving equilibrium.</p></li>
	<li><p style="border: none; padding: 0cm"><span style="display: inline-block; border: none; padding: 0cm"><strong>Approach
	through application:</span></strong><br/>
For example, if H1 and H2
	(energy as transferred from surface to object on day or at dark
	times), their net effect is balanced via H1 = -H2 or another similar
	relationship.</p></li>
</ol>
<p style="border: none; padding: 0cm">Thus, the idea reduces global
temperatures by making energy balance of transfers during light
periods with dark periods using surfaces radiative transfers.</p>
<p style="border: none; padding: 0cm">To reduce global temperatures
by utilizing &quot;night&quot; cooling of radiant energy from space,
we aim to balance the energy transfer between day and night at
various stages through surface radiation.</p>
<h3 class="western" style="border: none; padding: 0cm">Step-by-Step
Explanation:</h3>
<ol>
	<li><p style="margin-bottom: 0cm; border: none; padding: 0cm"><span style="display: inline-block; border: none; padding: 0cm"><strong>Identify
	Key Concepts:</span></strong></p>
	<ul>
		<li><p style="margin-bottom: 0cm; border: none; padding: 0cm">Consider
		energy transitions during different phases (day and night).</p></li>
	</ul>
	<li><p style="margin-bottom: 0cm; border: none; padding: 0cm"><span style="display: inline-block; border: none; padding: 0cm"><strong>Understand
	Terms:</span></strong></p>
	<ul>
		<li><p style="margin-bottom: 0cm; border: none; padding: 0cm">&quot;night&quot;
		might indicate transition from light to dark or vice versa over
		time.</p></li>
	</ul>
	<li><p style="margin-bottom: 0cm; border: none; padding: 0cm"><span style="display: inline-block; border: none; padding: 0cm"><strong>Analyzing
	Radiation Transfer:</span></strong></p>
	<ul>
		<li><p style="margin-bottom: 0cm; border: none; padding: 0cm">Energy
		transfers in surface cooling across days and at nights can be
		balanced appropriately.</p></li>
	</ul>
	<li><p style="margin-bottom: 0cm; border: none; padding: 0cm"><span style="display: inline-block; border: none; padding: 0cm"><strong>Key
	Point:</span></strong></p>
	<ul>
		<li><p style="border: none; padding: 0cm">Achieving energy
		equilibrium by balancing radiant transfer effects between day and
		night via surfaces.</p></li>
	</ul>
</ol>
<p style="border: none; padding: 0cm">Thus, the idea helps us to
balance radiation flows during different times phases through surface
cooling to reduce global temperature effectively.</p>