GC048-02
Stratospheric Aerosol Climate Intervention Designed to Minimize Negative Impacts
Abstract:
We use the NCAR Community Earth System Model, version 2, using the Whole Atmosphere Community Climate Model version 6, for simulations using feedback control on sulfur emissions to the stratosphere, with impacts as metrics. Because this state-of-the-art model includes complete treatment of diffuse radiation, aerosols, and atmospheric chemistry, as well as built in simulations of crop production, it is ideal for this purpose. We know that if warming from greenhouse gases is countered with reduction of solar radiation to cancel out the globally-averaged radiative forcing, the planetary temperature can be kept from changing, but the hydrological cycle will be weaker, with a reduction of globally-averaged evapotranspiration and precipitation, particularly in summer monsoon regions. Temperature, precipitation, and insolation changes, as well as enhanced ultraviolet radiation, enhanced diffuse radiation, changes of surface O3 concentration, and CO2 will all impact crops. We start by examining previous simulations to develop a transfer function between stratospheric aerosol loading and various metrics of agricultural productivity. These include global caloric intake from major crops, as well as regional food availability. For model runs that did not include a crop model in the past, we use the Community Land Model offline, driven by climate model output.