chapter_16 - Hurricanes Hurricanes This chapter discusses:...

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Unformatted text preview: Hurricanes Hurricanes This chapter discusses: 1. Tropical cyclone and hurricane development, Tropical structure, and movement structure, 1. Hurricane damages, warning systems, and naming Hurricane conventions conventions Tropical Weather & Waves Tropical Tropical winds Tropical typically blow from the east, and when they encounter a slow moving trough of low pressure, called a tropical wave, the winds initially converge and lift to produce showers and thunderstorms. thunderstorms. Figure 16.1 Structure of a Hurricane Structure Tropical cyclones are Tropical the international name of hurricanes, which typically form from an organized mass of storms formed along a tropical wave. along In this image of In Hurricane Elena, the central area of broken clouds is the eye, surrounded by an eye wall cloud and spiral rain bands, with a total diameter nearing 500 kilometers. 500 Figure 16.2 Hurricane Wind Profile Hurricane Figure 16.3 The low pressure core of the hurricane is surrounded by several The thunderstorms, each with updraft and downdraft cycles. thunderstorms, The wind and moisture cycle is repeated as: surface moist air converges in a counterclockwise pattern at the eye, surface rises to create high pressure aloft, condenses, precipitates, dries, diverges outward in a clockwise pattern, sinks, and warms. diverges 3-D Radar Image of Hurricane 3-D Figure 16.4 Several key features of a hurricane are shown in this radar Several composite image, including overshooting clouds, the area of strongest echoes (heaviest rain), and the eyewall. strongest Formation by Organized Convection Formation Figure 16.5A Figure 16.5B One theory explains that hurricane formation requires cold air above an One organized mass of thunderstorms, where the release of latent heat warms the upper troposphere, creates high pressure aloft, which pushes air outward and causes a low to deepen at the surface. outward Air moving toward this low intensifies the cycle. Formation by Heat Engine Formation Another theory of hurricane development proposes that Another a heat engine cycle, fueled by warm moist input air and the release of heat when it converts to cool dry air. the Differences in the input and output temperatures Differences determine the amount of work on the ocean and winds that is performed. that Hurricane Stages of Development Hurricane The initial The components of a hurricane may form as a tropical disturbance, grow into a tropical depression when winds exceed 20 knots, become a tropical storm when winds exceed 35 knots, and finally then qualify as a hurricane when winds exceed 64 knots. knots. Figure 16.6 Hurricane Movement Hurricane Global patterns of Global tropical cyclone formation and movement have been recorded on this figure, which notes regional names for these systems. these Travel speeds for Travel the hurricane my range from 10 to 50 knots, but they may also stall over a region and cause destructive flooding. destructive Figure 16.7 Erratic Paths of Hurricanes Erratic Figure 16.8 Historical charts of hurricane location may reveal erratic, and hard to predict, patterns of movement. erratic, As this figure shows, hurricanes may occasionally As double back. double Further, when removed from the ocean and without a Further, moisture source to supply energy, they may still continue an inland journey. continue In the North Atlantic, on average 3 storms per year In move inland and bring damaging winds and rain. move North Atlantic Hurricanes North Composite infrared Composite imagery of Hurricane Georges reveals the pattern of a seasonal threat for Central and North America coastlines. coastlines. Tropical cyclones at Tropical the same latitude survive longer in the Atlantic than Pacific Ocean because of warmer Atlantic Ocean waters. waters. Figure 16.9 Hurricane Damage & Warning Hurricane Figure 16.11 Figure 16.10 Hurricanes have their highest wind speeds on the side where Hurricanes storm pushing winds amplify cyclonic, or counterclockwise, rotational winds. In coastal areas, flooding is aggravated by the hurricane low pressure triggering higher tides and Ekman transport piling up water. transport Hurricane Watch & Warning Hurricane Figure 16.5A The National Hurricane Center in Florida issues a hurricane watch 24 to The 48 hours before a threatening storm arrives, and if it appears that the storm will strike within 24 hours, a hurricane warning is issued. storm While some consider the warning area too large, causing unneeded While evacuation, such evacuations have saved many lives. evacuation, Hurricane Hugo, with peak winds near 174 knots, caused tremendous Hurricane damage. damage. Hurricane Saffir-Simpson Winds Hurricane Figure 16.13A Figure 16.14 In 1989 Hugo caused nearly $7 billion in damages in the U.S., In killing 49 in the Caribbean and United States. Current classification of hurricanes is based on their wind speed, however, and not on human or property damage. however, Hurricanes range from category 1 to 5, with winds of 64 to more Hurricanes than 135 knots. than Hurricane Names and Cost Hurricane Category 5 Hurricane Category Andrew (1992) was the costliest US storm, but it ranks as less intense than 1935 and 1969 hurricanes. 1969 Hurricane names are Hurricane chosen from an alphabetical list of male and female names for the Atlantic and Pacific, some of which are retired if the storm was especially damaging. especially Figure 16.14 Hurricane Andrew Devastation in Homestead, Florida August 24, 1992 August Figure 16.15 Likelihood for Landfall Likelihood Between 1900 and Between 1999, only two category 5 hurricanes have made landfall along the Gulf or Atlantic. Atlantic. Numerous Numerous category 1, and less damaging storms, that do make landfall may not cause much damage, but bring needed rainfall. needed Figure 16.16 ...
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This note was uploaded on 03/15/2010 for the course ATOC ATOC 250 taught by Professor Gyakum during the Spring '09 term at McGill.

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