But why all the fuss anyway about some hot water in the tropical Pacific Ocean? Well, it's not just the hot water. It's also the hot air. Try this: take two cups that are the same. Fill one with cool water. Fill the other with hot water. (Not boiling, just good and hot.) Place them on a table. Hold each of your hands over one cup and feel the difference in the air above the water. (Don't actually touch the water. Just feel the air.) The hot water warms the air above it. The cool water doesn't. Now, imagine you fill your bathtub with hot water. Think about how warm and steamy the air in the bathroom gets. Now, imagine millions and millions of bathtubs-ful of hot water. All of that moist, hot air has to go somewhere. Scientists know that hot air rises and carries the moisture with it. Once the moisture gets into the air and starts to cool, rainclouds start to form. |
Now try this: hold a small mirror
over the cup of hot water for a few minutes. The moisture in
the air should collect on the mirror, and, as it cools, form
tiny droplets. Imagine the bathroom mirror after
you fill the bathtub with hot water. The "water" on the
mirror is caused by the water vapour in the air gathering
and cooling. Now imagine the air over the hot water of the
tropical Pacific Ocean. Huge rainclouds start to form and
flooding results in South American countries along the
coast.
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