Subtropical anticyclone is an essential component of the atmospheric circulation in the subtropics, and it is responsible for the formation of subtropical monsoons and deserts. There are two subtropical anticyclones in the subtropical northern hemisphere in boreal summer, and three subtropical anticyclones in the subtropical southern hemisphere in austral summer. These five summertime subtropical anticyclones are all located at the lower troposphere over the subtropical oceans.
To assess the possible responses of the subtropical anticyclones to greenhouse gases (GHG) forcing, Dr. HE Chao from China Meteorological Administration, and Drs. WU Bo, ZOU Liwei and Prof. ZHOU Tianjun from CAS Institute of Atmospheric Physics adopted multiple metrics and obtained robust results. Coupled models under GHG forcing show that the subtropical anticyclones over North Pacific, South Atlantic and South Indian Ocean will become weaker in future under RCP8.5 scenario, whereas the subtropical anticyclones over North Atlantic and South Pacific will become stronger.
"Intensity change of the subtropical anticyclones to GHG forcing is dominated by two factors -- the enhanced tropospheric static stability and the pattern of change in diabatic heating", said Dr. HE. "The tropospheric static stability is enhanced via moist adiabatic adjustment under GHG forcing, and it acts to reduce the intensity of all the subtropical anticyclones. Meanwhile, the pattern of change in the tropospheric diabatic heating acts to weaken the North Pacific subtropical anticyclone but to enhance the subtropical anticyclones over North Atlantic and South Pacific."
"Our findings show evidences that the global warming will have different impacts on the global subtropical anticyclones", said Dr. ZOU Liwei, the co-author of the paper. "The intensity of North Pacific subtropical anticyclone reduces significantly, since both the enhanced static stability and enhanced diabatic heating act to weaken it. Over South Atlantic and South Indian Ocean, the effect of enhanced static stability dominates, and the subtropical anticyclones over these two basins also become weaker. The effect of reduced diabatic heating overwhelms the effect of enhanced static stability over North Atlantic and South Pacific, and their combined effect enhances these two subtropical anticyclones."
This study is recently published in Journal of Climate.