# Describe the relationship between atmospheric pressure and wind speed in a hurricane

### Understanding Barometric Pressure in Hurricanes | Rhino Steel Building Systems

Get Prepared · Lightning Safety · Tornadoes · Watches and Warnings · Hurricane Preparedness · Flash Floods The wind blows because of differences in air pressure from one location to What is Air Pressure? Meteorologists can forecast the speed and direction of wind by measuring air pressure with a barometer. Wind speed and air pressure, also called barometric pressure, are closely The high winds in a hurricane are due to the extreme low pressure at the The violent winds of a tornado correspond with a highly localized pressure minimum. of barometric pressure to explain the current and forecast weather. How Air Pressure Affects the Strength of a Hurricane cyclone or the highest wind speed, weather specialists know the pressure indicates whether a hurricane is weakening or strengthening. What Is Barometric Pressure? A photo of Hurricane Irma shot from space is superimposed with the text "Barometric.

The classical Dvorak [ 23 ] developed a Current Intensity CI estimates that can be determined subjectively or objectively using satellite images. The wind-pressure relationship provides a critical analysis tool for obtaining the maximum wind speed based on MSLP.

The actual practice of Dvorak technique varies in different operational centers. Some centers use Dvorak technique to estimate the maximum wind speed, and then use wind-pressure relationship to obtain the MSLP [ 4 ]. Therefore, the wind-pressure relationship is essentially in the assessment of TC intensity. Many wind-pressure relationships were derived based on the cyclostrophic wind equation: A loose approximation was applied in the actual practice; the relationship was given in the form of 2 Where Vmax is the maximum wind, penv is the environmental pressurea and n are empirical constants.

The relationships were changed by varying the values of a and n [ 5 - 11 ].

## Severe Weather

Among these relationships, the most widely used in the west North Pacific was derived by Atkinson and Holliday [ 10 ] here after AH Aside from the development of CI number, Dvorak [ 23 ] suggested a table describing the wind-pressure relationship, which was used in some operational centers such as the National Hurricane Center NHC. The wind-pressure suggested by Koba et al.

Current studies pointed that TCs are well approximated by the gradient wind balance [ 1314 ]: Based on the wind balance, Knaff and Zehr [ 15 ] developed a comprehensive reconsideration of windpressure relationship, which considered the effect of TC size, latitude, translation speed, and environmental pressure on the relationship: Holland [ 16 ] presented a new technique for the wind-pressure relationship. Together with a method of objectively determining a derivative of the Holland b parameter, which relates directly to surface winds and varies with the pressure drop into the cyclone center, intensification rate, latitude, and translation speed.

The relationships of Knaff and Zehr [ 15 ] and Holland [ 16 ] provide a realistic scatter in the maximum wind speed for a given MSLP, which are better than traditional approaches that provide a unique wind for each central pressure. Since the recent studies related to the wind-pressure relationship by Knaff and Zehr [ 15 ] and Holland [ 16 ] are based on the best-track data and aircraft data for TCs primarily in the Atlantic, the wind-pressure relationship for TCs in the western North Pacific are need to be examined.

The storm is approximately km mi in diameter, which is about average for hurricanes.

The area of broken clouds in the center is its eye. Elena's eye is almost 40 km 25 mi wide. Within the eye, winds are light and clouds are mostly broken. The surface pressure is very low, nearly mb.

## Understanding Barometric Pressure in Hurricanes

Hurricane Elena as photographed from the space shuttle Discovery during September, Structure of a Hurricane Notice that the clouds align themselves into spiraling bands called spiral rain bands that swirl in toward the storm's center, where they wrap themselves around the eye.

Surface winds increase in speed as they blow counterclockwise and inward toward this center. Adjacent to the eye is the eye wall, a ring of intense thunderstorms that whirl around the storm's center and extend upward to almost 15 km 49, ft above sea level. Notice that the cloud tops in the eye wall region extend above the other clouds. Within the eye wall we find the heaviest precipitation and the strongest winds.

Figure K shows a top-down view of a typical hurricane.

All strong tropical cyclones consist of the following components: All tropical cyclones rotate around an area of low atmospheric pressure near the Earth's surface.

The pressures recorded at the centers of tropical cyclones are among the lowest that occur on Earth's surface at sea level. Tropical cyclones are characterized and driven by the release of large amounts of latent heat of condensation as moist air is carried upwards and its water vapor condenses. This heat is distributed vertically, around the center of the storm. Thus, at any given altitude except close to the surface where water temperature dictates air temperature the environment inside the cyclone is warmer than its outer surroundings.

A strong tropical cyclone will harbor an area of sinking air at the center of circulation. Weather in the eye is normally calm and free of clouds however, the sea may be extremely violent. The eye is normally circular in shape, and may range in size from 8 km to km 5 miles to miles in diameter.

In weaker cyclones, the clouds may cover the circulation center, resulting in no visible eye. The eyewall is a circular band of intense convection and winds immediately surrounding the eye. It has the most severe conditions in a tropical cyclone.

How do hurricanes form over the Atlantic Ocean

Just like an acrobat with two people stacked on his shoulders would want to move to where there wasn't so much pressure on him, air moves from areas where the pressure is higher to where it is lower. What causes Air Pressure? Air pressure depends on the density of the air, or how close together its molecules are.

You know that a hard rubber ball is more dense than a Styrofoam ball and that ice cream is more dense than whipped cream. Air lower in the atmosphere is more dense than air above, so air pressure down low is greater than air pressure higher up.

Remember those acrobats; there's a lot more pressure on the one on bottom than on the one on top.

### What is the relationship between air pressure and wind? | Yahoo Answers

Temperature also makes changes in air pressure. In cold air, the molecules are more closely packed together than in warm air, so cold air is more dense than warm air. Rising and Sinking Air Since warm air is less dense and creates less air pressure, it will rise; cold air is denser and creates greater air pressure, and so it will sink.

When warm air rises, cooler air will often move in to replace it, so wind often moves from areas where it's colder to areas where it's warmer.