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February 20, 2014 - Haze over India and Bangladesh
Haze over India and Bangladesh Image used for Spacing Purposes
Satellite: Terra
Date Acquired: 2/5/2014
Resolutions: 1km (364.2 KB)
500m (1.3 MB)
250m (3.3 MB)
Bands Used: 1,4,3
Credit: Jeff Schmaltz
MODIS Land Rapid Response Team,
NASA GSFC

In what has become common in Bangladesh during the winter, thick haze blanketed the country when the Moderate Resolution Imaging Spectroradiometer (MODIS) aboard the Terra satellite acquired this true-color image on February 5, 2014.

The hazy pall is the product of large numbers of fine solid and liquid particles drifting in the atmosphere. These aerosols scatter or absorb sunlight depending on the composition and shape of the particles. Landscape colors that would normally be vibrant and distinct become an opaque shade of gray. The white patches in the image are clouds.

The aerosol particles have a variety of sources, but biomass burning plays an important role in Bangladesh, where a significant portion of the population relies on traditional fuels such as week, straw and dung for cooking and for heating homes. These organic fuels deliver a heavy load of particles to the atmosphere because people tend to burn them at relatively cool temperatures; this leads to incomplete combustion.

Vehicle traffic and industry also contribute to the winter haze over Bangladesh. The brick industry, which mainly operates in the winter, is a major source of particles because most brick makers in the region rely on inefficient fixed-chimney kilns rather than cleaner-burning Hoffman or zig-zag kilns. According to one study based on data from ground-based air quality sensors, about one third of the find particulate pollution come from motor vehicles, one third from brick kilns, and the rest from winds blowing dry soil and road dust.

While brick production and heating needs increase significantly during the winter, meteorological conditions also play a role in building the haze. During the rest of the year, heavy rains help wash pollution particles from the air; but the winter months tend to be dry. Winds are also weaker in the winter, which leads to less movement and convection in the atmosphere.

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