Black Carbon Contributes To Droughts And Floods In China

In a paper appearing in the September 27 issue of SCIENCE, Surabi Menon of NASA and Columbia University, New York, and her colleague, James Hansen of NASA's Goddard Institute for Space Studies, New York, indicate black carbon can affect regional climate by absorbing sunlight, heating the air and thereby altering large-scale atmospheric circulation and the hydrologic cycle.

Using the NASA Goddard Institute for Space Studies climate computer model and aerosol data from 46 ground stations in China, Menon and Hansen conducted four sets of computer simulations to monitor the effects of black carbon on the hydrologic cycle over China and India. The aerosol data from the Chinese ground stations were provided by Yunfeng Luo, a co-author on the study from the Institute of Atmospheric Physics, Chinese Academy of Sciences.

In the four numerical simulations, Menon and Hansen isolated specific factors such as sea surface temperature, other greenhouse gases and aerosols, and analyzed whether changes in those factors would be responsible for hydrologic cycle changes.

Out of the four scenarios, the effect of increased amounts of soot (over southern China) created a clear tendency toward the flooding scenario that has been occurring in southern China and the increasing drought over northern China that has persisted over the last several years

"If our interpretation is correct, then reducing the amount of black carbon or soot may help diminish the intensity of floods in the south and droughts in the northern areas of China, in addition to having human health benefits," Hansen said. Currently research is being conducted to verify a similar pattern over India.

Black carbon or soot is generated from industrial pollution, traffic, outdoor fires and household burning of coal and biomass fuels. Soot is a product of incomplete combustion especially of coal, diesel fuels, biofuels and outdoor biomass burning. Emissions are large in China and India because cooking and heating are done with wood, field residue, cow dung, and coal, at a low temperature that does not allow for complete combustion. These resulting soot particles absorb sunlight, just as dark pavement becomes hotter than light pavement in the summertime.

When soot absorbs sunlight it heats the air and reduces the amount of sunlight reaching the ground. The heated air makes the atmosphere more unstable, creating rising air (convection), which forms clouds and brings rainfall to regions that are heavily polluted.

The increase of rising air in southern China is balanced by an increase of sinking air (subsidence) and drying in northern China. When air sinks, clouds and thus, rain cannot form, creating dry conditions. For example, deserts are places where subsidence occurs.

In recent years, northern China has suffered from an increased severity of dust storms, while southern China has had increased rainfall that is thought to be the largest change in precipitation trends since the year 950. Menon and Hansen believe that human-made sunlight-absorbing aerosols may be responsible.

This research continues long-term observations of global climate change and was funded by NASA's Earth Science Enterprise and the National Science Foundation. NASA's Earth Science Enterprise is dedicated to helping us to better understand and protect our home planet.