00:01
All righty, we've got a pretty realistic problem here.
00:02
Global warming is a serious issue, and it has been shown to produce rising sea levels, partly due to the fact that there's the melting ice caps, and also partly due to the expansion of water as the average ocean temperature rises.
00:19
So to get some idea of this effect, what we want to do is calculate the change in length of a column of water.
00:27
That is one kilometer high.
00:29
So we're going to say we have a length equal to one kilometer.
00:35
And it has a temperature increase at delta t equal to one degree celsius.
00:42
And we want to assume that the calm is not free to expand sideways, which as a model for the ocean, this is very reasonable because the ocean is really only going to expand sideways as it gets closer to the shore.
00:53
And at that point, also only to a very limited degree.
00:57
And also, to help with this approximation, we're going to neglect the fact that the ocean warming is not uniform with depth.
01:08
So, first of all, we need to find the coefficient of linear thermal expansion of water because we are assuming that the water is constrained to a cylinder, but unconstrained in length.
01:20
So we can find that from a wide variety of sources to actually find that coefficient.
01:29
So let's start here...