So class='bold'>temperature goes up, solubility goes up.

Snow, ice... class='bold'>temperature 23 class='bold'>below freezing.

class='bold'>Temperature 44.2.

They'll say delta S of the environment is equal to the class='bold'>heat or, let me say, the class='bold'>heat absorbed by the environment, divided by the class='bold'>temperature of the environment.

I warned you about the class='bold'>heat, but you don't listen!

Well, I got two words for you class='bold'>Heat syndrome.

I know it was supposed to be very warm there, but...

It would be a shame to let a few class='bold'>degrees of temp... ...class='bold'>temperature interrupt us.

Some dark night when her back is turned, I'll snatch her class='bold'>thermometer and plunge it between her shoulder blades.

It's a little couple paragraphs to explain why we call that unit of class='bold'>heat the watt, and where he got his inspiration.

Article 36 Consideration of reports

True marble is the metamorphic form of limestone produced by class='bold'>heat and pressure.

You may not care if you die from class='bold'>heat but becoming a piece of beef jerky is not a lifelong ambition of mine.

Since it tends to get hot, it's covered by a piece of metal called a class='bold'>heat sink, which draws class='bold'>heat away from the processor.

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If the vertical class='bold'>class='bold'>temperature gradient is 12.9 C per 100 meters (where the positive sign means class='bold'>temperature gets hotter as one goes higher) then horizontal light rays will just follow the curvature of the Earth, and the horizon will appear flat.

Shallow ponds often have a continuous class='bold'>class='bold'>temperature gradient from warmer waters at the surface to cooler waters at the bottom.

We know that the angles of a triangle x class='bold'>degrees plus y class='bold'>degrees plus z class='bold'>degrees are equal to 180 class='bold'>degrees.

Horizontal gradient

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There is a scaling.

This is going to be equal to 75 class='bold'>degrees 60 class='bold'>degrees which is equal to 135 class='bold'>degrees

That every time that we said, OK, a change in entropy from here to here is the class='bold'>heat absorbed by a reversible process divided by the class='bold'>temperature at which it was absorbed.

So let's say that this is 0 Celsius, that is 1 Celsius, 2 Celsius, 3 Celsius.

So the 60 class='bold'>degrees 75 class='bold'>degrees

The measures of its angles are, 30 class='bold'>degrees, 60 class='bold'>degrees and 90 class='bold'>degrees.

So the general rule of thumb is, if you're dealing with a solid in a liquid solvent, lowering the class='bold'>temperature will decrease the solubility, because it's harder to jam the molecules in there, and increasing the class='bold'>temperature will increase the solubility.

Vertical gradient

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class='bold'>Hierarchy Establishment of Courts

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90 class='bold'>degrees west 1 class='bold'>degree south

It's only a little over a hundred.