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 10: Smoke and Fires

Fire Detection and Monitoring using Satellite Observations

The figure below is a visible image taken from a weather satellite on August 16, 1996 . You generally don't see visible images on the nightly news because the sun has set by 10:00 PM and so it is dark over the United States. This image was made during the daylight hours. Notice the smoke plumes. The fires are marked by red boxes. This was a bad summer for fires in the west because of dry summer weather, and wet weather in the spring. Continue reading to learn how we know where the fires are located.

Observations of electromagnetic radiation with a wavelength of approximately 4 micrometers are used by scientists and weather forecasters to detect fog at night and to measure the temperature of the ocean during the night. Fires are evident in an image of data collected by an instrument that observes radiation with a wavelength of 4 micrometers. The fires show up as 'hot spots', and in the image below this is denoted by the red squares.

Scientists use observations at 4 micrometers to monitor biomass burning in North and South America.

Why do you think it would be better to use observations at 4 micrometers rather than the visible wavelengths(visible light has a wavelength between .4 and .7 micrometer)?

More on monitoring fires from space.



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