Local and convected rates of change

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Homework Statement


This is less of a help me answer something question more a help me understand this question.

I was reading though my hydrodynamics notes and there was a derivation that ended up with the follow equation
\frac{D\psi}{Dt} = \frac{\partial\psi}{\partial{t}} + (\underline{u}.grad)\psi
now i completely understood the derivation, what I don't understand is the result why doesn't \frac{D\psi}{Dt} = \frac{\partial\psi}{\partial{t}}? Also what do the capital D even mean?

Homework Equations





The Attempt at a Solution

 
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Thread 'Use greedy vertex coloring algorithm to prove the upper bound of χ'
Hi! I am struggling with the exercise I mentioned under "Homework statement". The exercise is about a specific "greedy vertex coloring algorithm". One definition (which matches what my book uses) can be found here: https://people.cs.uchicago.edu/~laci/HANDOUTS/greedycoloring.pdf Here is also a screenshot of the relevant parts of the linked PDF, i.e. the def. of the algorithm: Sadly I don't have much to show as far as a solution attempt goes, as I am stuck on how to proceed. I thought...
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