MadSci Network: Earth Sciences |
That's a good question! I believe that I can offer several possibilities. Firstly, the sand in Cancun is, I believe, composed of broken up shell material with some mix of sand, silt and clay. The finely broken up shell material is called "coquina". Coquina shell fragments are light- colored, angular and often contain small holes called pores. This means that they 1) reflect sunlight more than a darker material would, thus absorbing less energy to turn into heat, and 2) have a greater surface area as compared to total mass than a round grain would have. This means that they have a greater surface area to release heat through. Finally, the coquina material tends to "wick" moisture up more than a round, solid grain would, and as the water evaporates the fragment cools down. On the other hand, the sand in Connecticut or New York is more likely to be composed of rock fragments and rounded sand grains, as well as a greater percentage of silt and clay. These sedments are more likely to be dark colored than the coquina and thus more likely to absorb sunlight to turn into heat. The grains are also more likely to be less porous (ie with less holes in them) and more rounded. This means in turn that when this material lies at the surface of the beach it is 1) less likely to absorb water and give off heat by evaporation, and 2) has a smaller surface area as compared to total mass than the coquina. These characteristics mean that the Connecticut or New York sands will tend to be and stay, hotter. I hope this helps. regards JM Munsil, PG
Try the links in the MadSci Library for more information on Earth Sciences.