The Coolest Mixing Process in the Ocean
MIRJAM SOPHIA GLESSMER (mirjam.glessmer@tuhh.de) is coordinator of teaching innovation in the Center for Teaching and Learning, Hamburg University of Technology, Hamburg, Germany.
For example, salt fingering happens in certain parts of the world's oceans where warm, salty water occurs above cold, fresh water. "Warm" and "cold," "salty" and "fresh" are relative terms here — in the ocean "warm" water might only be a tenth of a degree warmer than "cold" water and "salty" water might not differ very much from "fresh," either. The most important part here is that the water on top — even though higher in salinity — must have a lower density than the water at the bottom. This means that the differences in temperature and salinity should be such that the influence of temperature on density is larger than that of salinity.
You can easily watch this kind of mixing in a mesmerizing experiment:
Take a large, clear container and fill it with cold, fresh water. Leave enough space in the container so it won't overflow later! Then take a small, clear bottle (ideally one you can close off with your thumb) and fill it to overflowing with water as hot as you can bear to touch. Add a couple of drops of food dye and shake well. In this experiment, we replace salt with food dye because its influence on density is similar enough and, in contrast to "real" salt, we can watch how it slowly mixes into the fresh water!
Now insert the bottle into the large, clear container and lay it on its side on the bottom of the container. Some of the hot water is going to flow out and rise to the surface of the larger container. The rest will be trapped inside the little bottle. Now you have created two interfaces between hot water and cold water, one near the surface of the large container and one inside the small bottle, and you will quickly see salt fingers forming.
As you watch the dye slowly mixing throughout the whole volume of water, you can also feel the temperatures adjusting to each other by sliding a finger carefully down the sides of the container.
Salt fingering happens over large volumes of the ocean and has important effects in the subtropical gyres, for example, where it supplies nutrients from the deeper ocean to the nutrient-depleted surface ocean. Salt fingers are larger there than in our experiment, and the whole process happens more slowly because the differences in temperature and salinity are much smaller.
You can also do this experiment on a larger scale, while carefully measuring temperature and salinity, but the small-scale experiment is a lot easier to set up and repeat as needed and anyone watching the experiment is guaranteed to be fascinated and keen to learn more about ocean physics.
ADDITIONAL RESOURCES
For more information on this and other experiments, check out my blog "Adventures in Oceanography and Teaching" at http://mirjamglessmer.com/blog.