Last update: September 17th, 2019 at 8:00 am
A winter temperature inversion likely contributed to the widespread haze the Moderate Resolution Imaging Spectroradiometer (MODIS) on NASA’s Aqua satellite observed on January 18, 2010. The gray-brown haze extends from Beijing to the South China Sea from north to south and from Korea to central China from east to west (shown in the large image). This image shows the densely populated and industrialized North China Plain between Beijing and the Yangtze River, where the haze is so dense that it completely obscures the ground.
The haze hangs low over the ground, where it poses a health hazard. Higher elevation peaks rise above the thick air, and clouds are clearly above the haze. In the west, white fog or low cloud mingles with the haze. The fog or low cloud is white in contrast to the gray tone of the haze.
Winter temperature inversions trap a layer of cold air beneath a layer of warm air. The air near the ground cannot rise and mix with the rest of the atmosphere. This means that pollutants build up near the surface until the inversion lifts. In China, most of the pollutants are released from burning coal for power and heat.
Credit: NASA image courtesy the MODIS Rapid Response Team at NASA GSFC. Caption by Holli Riebeek.