Lesson 1
Meteorological Satellite Orbits
Lesson 2
Review of Radiative Transfer
Lesson 3
Visible Image Interpretation
Lesson 4
Infrared Image Interpretation
Lesson 5
Multispectral Image Interpretation
Lesson 6
Fires & Aerosols
Lesson 7
Winds
Lesson 8
Sounders
Lesson 9
Fog and Stratus
Lesson 10
Thunderstorm
Lesson 11
Energy Budget
Lesson 12
Hurricanes
Lesson 13
Global Circulation
Lesson 14
Synoptic Scale
Lesson 15
Local Circulation
Lesson 16
Satellite Oceanography
Lesson 17
Precipitation

Lesson 12: Background

Hurricanes (Huracan is the Taino god of the wind) and typhoons (Taifung is Chinese for "great wind") are both tropical cyclones; hurricanes occur in the Atlantic Ocean and typhoons in the Pacific Ocean. To qualify as a hurricane or typhoon a storm must have sustained winds exceeding 64 knots (74 miles per hour). Though the high winds inflict damage when these storms hit land, it is the huge waves, storm surge, and associated flooding that cause most of the destruction. These ferocious atmospheric storms cannot survive without the moisture supplied by warm ocean water. They are vivid examples of the coupling between the earth's oceans and atmosphere.

Tropical cyclones are large whirling storms that obtain their energy from warm ocean waters. They stand out on satellite photographs due to their circular cloud patterns and, in the stronger storms, a nearly clear eye at the center. The clarity and size of the eye on satellite images helps meteorologists estimate a cyclone's strength.

The surface pressure is related to the temperature of the

  1. The eye of hurricane Iris
  2. Dvorak technique
  3. Surface pressure and thermal structure
  4. Wake effects on water
  5. Microwave Observations of Hurricanes



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