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1 Introduction Whole atmosphere climate models resolve the interactions between atmospheric dynamics, chemistry, aerosols, and upper atmosphere physics, and are needed to study a wide range of scientific problems. This includes: stratospheric ozone loss (Solomon, 1999; Solomon et al., 1986), its recovery (Fang et al., 2019), and the potential limits of recovery due to future aircraft (J.
1 Introduction The adverse global impacts produced by human-induced surface warming are well-documented in over 30 years of previous scientific literature and international proceedings. In 1990, the first Intergovernmental Panel on Climate Change (IPCC) Assessment Report already highlighted many of the future challenges and laid the ground for the creation of the United Nations Framework Convention on Climate Change (UNFCCC).
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