cheezyWXguy wrote: BTW, what do they mean by low amplitude?
Any waveform has two basic characteristics...wavelength and amplitude (well, three actually - if you want to count frequency, but let's not go there). Whenever you hear mention of a "short wave" or "long wave" ridge or trough, the "wave" being referred to is short for "wavelength".
Essentially the amplitude is the "height" of the wave, or how much of a base to crest (usually, but not always entirely N-S or equator-to-pole) expanse the wave has.
Take the back of a 3x5 note card and turn it on its' side. Now take a pen or pencil and draw a line from the bottom left hand corner to the bottom right corner, making a small hill in the middle that goes about two inches from the bottom of the card - you just drew a simple low-amplitude "wave". Now do the same, but come within one inch of the top of the card - now what you have is a representation of a higher amplitude "wave".
There are a few other ways of looking at this. For example...a high amplitude wave puts a bigger N-S "dent" in the underside of the Atlantic ridge. In addition, it will generally be represented by a longer dashed line, since it is a "longer" inverted trough.
Hope I kept this simple enough - sometimes K.I.S.S. is not one of my strong points.