Environmental Research Letters 4 (2009), 045108. Coupled aerosol-size and chemistry–climate simulations show why constant forcing per unit injection is an approximation.
Chapter 7 of Climate change 2021: The Physical Science Basis, pp. 923–1054. §§7.3.2–7.3.3 contrast greenhouse-gas and aerosol effective radiative forcing.
Chapter 6 of Climate change 2021: The Physical Science Basis. Relevant sections are §6.3.1 for methane chemical and perturbation lifetime and §6.4.5 for climate–chemistry feedbacks.
Atmospheric chemistry and Physics 23 (2023), 13451–13467. Coupled chemical modelling distinguishes hydrogen leakage effects from accompanying changes in other precursor emissions.
PNAS 117 (2020), 1860–1866. Aircraft IO and particulate-iodine measurements constrain nonzero stratospheric iodine injection and multiphase recycling.
Atmospheric Chemistry and Physics 7, 1961–1971. DOI 10.5194/acp-7-1961-2007. The hygroscopicity parameter and dry diameter determine approximate activation properties.
Journal of the Atmospheric Sciences 34, 1149–1152. The theoretical droplet-number and shortwave-reflectance response is distinguished from absorption and subsequent cloud adjustments.
Journal of Geophysical Research 95, 1837–1851. Regional photochemical-model comparison of ozone precursor sensitivity in rural and urban environments.
Journal of Physical Chemistry 91, 433–436. The NASA abstract describes flow-system dimer production at 220–240 K and infrared/ultraviolet identification. Institutional record: ntrs.nasa.gov/citations/19870061046
Earth System Dynamics 7, 697–715. DOI 10.5194/esd-7-697-2016. A window-grey radiation model separates the blocking effect from the indirect solar-heating effect.
Chapter 7 of Climate Change 2021: The Physical Science Basis, pp. 923–1054. DOI 10.1017/9781009157896.009. Cited sections: emissions metrics and aerosol–cloud interactions; this institutional assessment is not an answer set for the Cambridge paper.
Annual Review of Earth and Planetary Sciences 37, 117–134. The physical ocean and solid-Earth portions distinguish fast exchange, slow ocean equilibration and a long carbonate/weathering tail. Biological mechanisms are outside the present expansion.
Cited physical-chemistry passages: Table 1, p. 119, and physical ocean/solid-Earth conclusions, p. 131.

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