# Great Pacific Garbage Patch Equilibrium Points

I was watching the science channel yesterday and the program mentioned the Great Pacific Garbage rim. I was struck by the illustration (and pretty much every subsequent animation/picture I've seen now has the same basic illustration) below:

Unless I'm not understanding something, the garbage swirls around in a huge closed trajectory and encloses two sinks ( the colorful swirly things; one on the left and one on the right). This isn't physically possible though, with the perfectly reasonable assumption that the tidal force field is continuously differentiable. Any closed curve has to enclose equilibrium points who's indices add to $+1$, but a sink has an index of $+1$ so this curve encloses a total of $+2$. There would have to be at least one other equilibrium point inside the closed trajectory that had an index of $-1$, so something like a saddle node:

But I can't find any illustrations showing any other equilibrium points other than these two. Does anyone know what they are, or perhaps if I'm not understanding something?

Theoretically, I agree that there should be one instable equilibrium point between the two stable equilibrium points when we have a 2D current field. However, there are some additional components of the problem:

• Ocean currents are not 2D but 3D currents. Considering only the sea surface might lets field lines disappear.
• The wind has an additional forcing. This is not true for all items and the wind already affects the ocean currents. However, litter items which are partly above the sea surface experience an additional wind forcing (see e.g. Yoon et al., 2010)
• Ocean currents are not time independent and equilibrium points may undergo a seasonal multi-annual cycling
• Accumulation zones are not necessarily stable equilibrium points but the residence time of the marine litter items in the named regions just needs to be sufficient long.
• The gyres are macroscopic accumulation regions. Thus, if we have regions with a higher density of particle trajectories and lower particles velocities we could identify these regions as accumulation regions from a macroscopic perspective.

About item three (Ocean currents are not time independent) I am not completely sure, but I think to remember an animation or plots in a publication which showed seasonal variations between the both garbage patches you showed.

As far as I remember the publications on that topic of global transport modeling of marine litter correctly, the eastern North Pacific Garbage patch is the actual accumulation region. It has a long tail towards west. Howell et al. (2012) writes about the North Pacific Gyre and plastic debris accumulation within it. I did not have time to read it in detail.

For further reading it might be interesting to look into these publications:

• Donovan Hohn's "Moby Duck" is a very good book about the garbage patch. It has two diagrams showing the gyres and current's etc. but the explanation in the book is better. Mar 28 '16 at 14:32
• Your first point about the three-dimensional nature of the ocean is key. Mar 28 '16 at 17:59
• Thanks @IsopycnalOscillation for the remark. Actually, I wasn't sure how relevant (and strong) upwelling and downwelling processes are in this specific region. Mar 29 '16 at 8:20

Yes, you're right, there should be (at least one) saddle point in the middle of the loop. And indeed, if you search for illustrations of Pacific ocean circulation, you can see the saddle point in some of them, like this one:

Source: Introduction to Tropical Meteorology, 2nd ed., chapter 3.3.1, fig. 3.20.

Now, in a lot of other maps, the saddle region is just left more or less blank. Apparently, that's because there just aren't any strong currents there; most of the circulation is going in a loop around both sinks (and the saddle), with only a relatively small fraction diverted into the middle. This illustration from Wikipedia is a good example:

Also, unlike sinks, saddle points in general won't accumulate debris; any flotsam on the surface will just float in along the stable axis, and then away again along the unstable axis. So even if there were strong surface currents in the region, you wouldn't expect any visible "garbage patch" there.

Besides, at least if you look closely enough, reality will almost certainly be more complicated, with multiple equilibrium points that shift over time. The following two maps (found on this page), although fairly old and probably of limited accuracy, may show a hint of the true complexity: