Suggested Searches

2 min read

Carbon Monoxide in Africa and Asia

Instruments:
Carbon Monoxide in Africa and Asia
December 12, 2004

The weather in the tropics is dominated by the tropical rain belt, which oscillates from the northern to the southern tropics over the course of the year. The tropical rain belt lies in the southern hemisphere roughly from October to March, and during this time the northern tropics experience a dry season in which precipitation is rare and biomass burning is frequent in regions like Central Africa (left) and Southeast Asia (right). Many of the fires are of human-made origin and serve the purpose of land-clearing and pasture and farmland renewal.

Burning of biomass releases large amounts of carbon monoxide (CO) into the atmosphere that are detected by the Measurements of Pollution in the Troposphere (MOPITT) remote sensing instrument on board the EOS satellite Terra. The image above shows the measured concentrations of CO at 700 millibars (roughly 2-3 km altitude) averaged over December 2-12, 2004. High concentrations of CO (color-coded in red) are seen over the biomass burning region, but the CO also spreads out over nearby oceans. Regions where no data are collected either due to clouds or high surface elevation (such as over the Himalaya) are colored in gray.

References & Resources

Image created by Jesse Allen, Earth Observatory using data provided courtesy of the NCAR and University of Toronto MOPITT Teams

You may also be interested in:

Stay up-to-date with the latest content from NASA as we explore the universe and discover more about our home planet.

Rare Snowfall in the Atacama Desert
4 min read

Snow infrequently falls in the high plains of northern Chile. And when it does, it doesn’t last for long.

Article
Senyar Swamps Sumatra
3 min read

A rare tropical cyclone dropped torrential rains on the Indonesian island, fueling extensive and destructive floods.

Article
Rings of Rock in the Sahara 
3 min read

In southeastern Libya, Jabal Arkanū’s concentric rock rings stand as relics of past geologic forces that churned beneath the desert.

Article