Stratospheric Dynamical Response and Ozone Feedbacks in the Presence of SO2 Injections. Issue 23 (7th December 2017)

• Record Type: Journal Article
• Authors: Richter, Jadwiga H.; Tilmes, Simone; Mills, Michael J.; Tribbia, Joseph J.; Kravitz, Ben; MacMartin, Douglas G.; Vitt, Francis; Lamarque, Jean‐Francois
• Is Part Of: Journal of geophysical research. Volume 122:Issue 23(2017)
• Page Start: 12, 557
• Page End: 12, 573
• Publication Date: 2017-12-07
• Subjects: SO2 injection -- geoengineering -- climate engineering -- climate modification -- stratosphere; Atmospheric physics -- Periodicals; Geophysics -- Periodicals; 551.5
• DOI: 10.1002/2017JD026912
• Languages: English
• ISSNs: 2169-897X

Abstract

Abstract: Injections of sulfur dioxide into the stratosphere are among several proposed methods of solar radiation management. Such injections could cool the Earth's climate. However, they would significantly alter the dynamics of the stratosphere. We explore here the stratospheric dynamical response to sulfur dioxide injections ∼5 km above the tropopause at multiple latitudes (equator, 15°S, 15°N, 30°S and 30°N) using a fully coupled Earth system model, Community Earth System Model, version 1, with the Whole Atmosphere Community Climate Model as its atmospheric component (CESM1(WACCM)). We find that in all simulations, the tropical lower stratosphere warms primarily between 30°S and 30°N, regardless of injection latitude. The quasi‐biennial oscillation (QBO) of the tropical zonal wind is altered by the various sulfur dioxide injections. In a simulation with a 12 Tg yr −1 equatorial injection, and with fully interactive chemistry, the QBO period lengthens to ∼3.5 years but never completely disappears. However, in a simulation with specified (or noninteractive) chemical fields, including O3 and prescribed aerosols taken from the interactive simulation, the oscillation is virtually lost. In addition, we find that geoengineering does not always lengthen the QBO. We further demonstrate that the QBO period changes from 24 to 12–17 months in simulations with sulfur dioxide injections placed poleward of the equator. Our study points to the importance of understanding and verifying of the complex interactions between aerosols, atmospheric dynamics, and atmospheric chemistry as well as understanding the effects of sulfur dioxide injections placed away from the Equator on the QBO. Key Points: SO2 injections cause the tropical lower stratosphere to warm primarily in the tropics, regardless of injection latitude Interactive chemistry changes significantly the shortwave heating in the stratosphere due to SO2 injections The period of the QBO lengthens due to equatorial SO2 injections and shortens due to injections poleward of the equator