If there is one characteristic that distinguishes us, as physicists, from the rest of humanity, it is the supreme confidence we have that we can make order-of-magnitude estimates. All we need is the back of an envelope or a cocktail napkin.
For example, we might consider Earth in its early days, when it was a molten sphere, and wonder what the period would be of oscillations between oblate and prolate shapes. We immediately note that the period could only depend on Earth’s density , its radius , and the gravitational constant . Dimensional analysis then reveals the remarkable result that must be of order , and not depend on at all. If we cannot remember the numerical value of , then we work in terms of the more familiar , the...
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