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Answer :
The pressure gradient is higher on the 5th at 7 am and the eye traveled approx. 400 miles with approx 17 mph.
What is a pressure gradient?
The pressure gradient, which is a physical parameter that represents the direction and rate at which pressure increases the most quickly at a certain area, is a term used in atmospheric science to describe the pressure gradient, which is common in the air but more generally of any fluid. In terms of pascals per meter (Pa/m), the pressure gradient is a dimensional quantity. It is, mathematically speaking, the gradient of pressure with respect to position. The force density is the name for the pressure gradient that is negative. Only the vertical depth of the column has any bearing on both the pressure gradient for any given true vertical depth and the vertical pressure of any point within its column. The path and geometry of the column are completely irrelevant.
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Final answer:
Hurricane storms are ranked on the Saffir-Simpson scale based on their wind speed. The closer the isobar lines on a map, the steeper the pressure gradient. Hurricane Fran hit the eastern coast of the United States in September 1996.
Explanation:
Hurricane storms are ranked on the Saffir-Simpson scale, where a category 5 rating is the most severe and category 1 is the least severe. The category of a hurricane is determined by its wind speed. For example, a category 5 hurricane has sustained winds of 157 mph or higher. Examples of category 5 hurricanes in the United States include Andrew, Camille, Katrina, Rita, Felix, and the "Labor Day" hurricane.
In early September of 1996, Hurricane Fran hit the eastern coast of the United States. The accompanying maps represent the location of Hurricane Fran at 7:00 AM EST on September 5 and 6. The small, black boxes extending southeast from the storm's center represent the location of the hurricane's eye at 6-hour intervals. The black lines are isobars, or lines of equal pressure, at 7:00 AM EST.
A steep pressure gradient is represented by a narrower spacing of isobar lines. This means that the pressure gradient of an area with isobar lines nearer to each other is steeper than an area with isobar lines with more space between them.
