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Evolution of Stratospheric Temperature and Ozone in GFDL Climate Model Simulations

John Austin and R. John Wilson. Evolution of Stratospheric Temperature and Ozone in GFDL Climate Model Simulations. AMTRAC: Description and runs. GFDL climate model, coupled chemistry 48L model, upper boundary ~ 0.002 hPa Horizontal resolution 2 x 2.5 deg. Finite Volume dynamical core

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Arctic ozone recovered - PowerPoint PPT Presentation

Evolution of Stratospheric Temperature and Ozone in GFDL Climate Model Simulations