Update README.md

README.md

@@ -30,7 +30,22 @@ 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 6 Qwen 1.5B models.
+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.
 
@@ -45,6 +60,10 @@ 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.
@@ -55,4 +74,229 @@ Temp of .4 to .8 is suggested, however it will still operate at much higher temp
 
 ---
 
+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>