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Hurricanes, cyclones, and typhoons are all the same weather phenomenon; we just use different names for these storms in different places. In the Atlantic and Northeast Pacific, the term “hurricane” is used. The same type of disturbance in the Northwest Pacific is called a “typhoon” and “cyclones” occur in the South Pacific and Indian Ocean. The ingredients for these storms include a pre-existing weather disturbance, warm tropical oceans, moisture, and relatively light winds. disaster wallpaper. If the right conditions persist long enough, they can combine to produce the violent winds, incredible waves, torrential rains, and floods we associate with this phenomenon.

So what makes a hurricane different from any other type of storm? Regular low pressure systems that bring us rain and snow, disaster wallpaper. whether they are over land or water, get their energy from the temperature difference surrounding them. That’s why it can be warm one day in the winter, a storm moves in with rain, and after the low pressure moves out, the temperature plunges.

Tropical systems occur in a warm, homogenous atmosphere, where temperatures don’t vary much. Tropical storms and hurricanes get their energy from warm ocean water. Ocean temperatures need to be 80 degrees or higher for a tropical system to maintain or gain strength. disaster wallpaper. That’s why the north Atlantic is called the “Hurricane Graveyard.” Hurricanes from lower latitudes that travel into the cool waters of the North Atlantic weaken quickly. Here’s another difference: Regular low pressure systems are attached to cold fronts and warm fronts, even over water. Tropical systems have no fronts attached to them. disaster wallpaper. Again, that’s because the temperatures around the storm are fairly uniform.