Typically, you must have ocean temperatures at a minimum of 80 degrees F as well as light winds in the upper atmosphere. Waves (areas of sharp change of winds at the surface) and other areas of low pressure (such as that along fronts) build convection (thunderstorms) over the center. As the convection builds, it creates updrafts in the center which draw in more energy to keep building the convection. The updrafts lower the pressure which, in turn, increases the winds. If there is a closed circulation (winds rotating around a point), you have a tropical system or cyclone.
Upper-level winds must be favorable to remove wasted energy but, at the same time, not be too strong to blow off the cloud tops or "suffocate" the storm preventing new energy from being processed. Warm waters typically provide rich, moist air above the water which is actually what the hurricanes use to survive. If there is no warm moist air, a storm cannot survive. This is why some systems (Tropical Storm Danny - late 90's, and Hurricane Katrina) have actually managed to survive over swampy areas without losing much intensity.
Wind shear is one of the most critical factors in controlling or even destroying hurricane formation, the more wind, the more powerful the hurricane. Conversely, if the wind is blowing in the opposite direction of the hurricane, it can slow it down or destroy it.
No, a bomb cannot destroy a hurricane formation. Hurricanes are massive, natural weather systems fueled by warm ocean water and atmospheric conditions. Attempting to disrupt a hurricane with a bomb would not be effective and could have harmful consequences.
The impact (destructive capability) happens as soon as the hurricane forms however the hurricane may never make landfall and therfore never cause damage to human property.
Hurricane Andrew was the first storm of the 1992 Atlantic hurricane season. The previous Atlantic hurricane was at the end of the 1991 season. Due to the unusual circumstances of its formation, this storm was never given a name. It is most widley known as the 1991 Perfect Storm. Had it been named, it would have been Hurricane Henri.
The lifespan of a hurricane can vary widely, but on average, they typically last about a week from formation to dissipation. This timeframe includes the period when the hurricane forms, intensifies, travels across the ocean, makes landfall, and eventually weakens and dissipates.
Wind shear is one of the most critical factors in controlling or even destroying hurricane formation, the more wind, the more powerful the hurricane. Conversely, if the wind is blowing in the opposite direction of the hurricane, it can slow it down or destroy it.
The warmer the water is the greater the potential for the formation or strengthening of a hurricane.
Energy plays a crucial role in the formation and intensity of a hurricane. Warm ocean waters provide the energy needed for a hurricane to develop and strengthen. As the warm air rises and cools, it releases latent heat energy, fueling the storm's circulation and increasing its intensity. The more energy available, the stronger the hurricane can become.
no a hurricane can not start another hurricane but it can start a tornado
No, a bomb cannot destroy a hurricane formation. Hurricanes are massive, natural weather systems fueled by warm ocean water and atmospheric conditions. Attempting to disrupt a hurricane with a bomb would not be effective and could have harmful consequences.
The sun provides the energy that drives the formation and intensification of hurricanes. As the sun heats the Earth's surface, warm air rises, initiating the circulation patterns that can lead to the development of a hurricane. The sun's energy also plays a role in evaporating water from the ocean, which is a critical component for hurricane formation.
The impact (destructive capability) happens as soon as the hurricane forms however the hurricane may never make landfall and therfore never cause damage to human property.
yes the air pressure changes
The National Hurricane Center (Miami, Florida) tracks the formation of these tropical storms. See the related link listed below for more information:
"Effects of Wind Speed on Tree Stability": investigate how different wind speeds affect the stability of various types of trees. "Hurricane Formation in a Bottle": create a model to demonstrate the process of hurricane formation using water, food coloring, and a spinning mechanism. "Comparing the Impact of Hurricane Categories on Building Materials": test different building materials to see how they withstand simulated hurricane conditions of varying categories.
Hurricane Andrew was the first storm of the 1992 Atlantic hurricane season. The previous Atlantic hurricane was at the end of the 1991 season. Due to the unusual circumstances of its formation, this storm was never given a name. It is most widley known as the 1991 Perfect Storm. Had it been named, it would have been Hurricane Henri.
The lifespan of a hurricane can vary widely, but on average, they typically last about a week from formation to dissipation. This timeframe includes the period when the hurricane forms, intensifies, travels across the ocean, makes landfall, and eventually weakens and dissipates.