Some features of this site are not compatible with your browser. Install Opera Mini to better experience this site.

Haze in Southwest China

Haze in Southwest China

Haze, clouds, and fog mingled in China’s Sichuan Basin on December 24, 2014, when the Moderate Resolution Imaging Spectroradiometer (MODIS) on NASA’s Terra satellite acquired this natural-color image. The haze obscured many features usually visible in satellite images of the area, including the city of Chongqing. In the eastern part of the basin, the tops of a series of ridges were visible despite the haze.

On the day this image was acquired, measurements from ground-based sensors at the U.S. Consulate in Chengdu reported PM2.5 measurements of 223 micrograms per cubic meter of air. Fine, airborne particulate matter (PM) that is smaller than 2.5 microns (about one thirtieth the width of a human hair) is considered dangerous because it is small enough to enter the passages of the human lungs. Most PM2.5 aerosol particles come from the burning of fossil fuels and biomass (wood fires and agricultural burning). The World Health Organization considers PM2.5 to be safe when it is below 25.

Haze in this region tends to worsen in the winter. In this case, the haze was likely trapped by a temperature inversion. Normally, air is warmest near the surface. Occasionally, a mass of warm air will move over cooler air so that the atmosphere actually warms with altitude. Since the cool air does not have the energy to rise through the warm air, vertical circulation slows and air becomes trapped near the surface.

Any pollutant that enters the air gets trapped as well, and haze builds up over time. Temperature inversions often form in basins and valleys because surrounding higher-elevation land helps contain cold air.

NASA image by LANCE/EOSDIS Rapid Response. Caption by Adam Voiland.

References & Resources