Biomass burning aerosols produce -2.5 W m^{-2} regional shortwave cooling over the South-East Atlantic, decomposed equally into ARI, ARI adjustments, and ACI after causal removal of confounding biases.
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The singular immersion freezing model applies only under limited cooling rates while the time-dependent approach integrates better with particle-based aerosol microphysics.
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Dissipating the correlation smokescreen: Causal decomposition of the radiative effects of biomass burning aerosols over the South-East Atlantic
Biomass burning aerosols produce -2.5 W m^{-2} regional shortwave cooling over the South-East Atlantic, decomposed equally into ARI, ARI adjustments, and ACI after causal removal of confounding biases.
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Immersion freezing in particle-based aerosol-cloud microphysics: a probabilistic perspective on singular and time-dependent models
The singular immersion freezing model applies only under limited cooling rates while the time-dependent approach integrates better with particle-based aerosol microphysics.