Land Cover Regulates the Spatial Variability of Temperature Response to the Direct Radiative Effect of Aerosols

Comparison of Effective Radiative Forcing Calculations Using Multiple Methods, Drivers, and Models

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Local temperature response to land cover and management change driven by non-radiative processes

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Why Does Aerosol Forcing Control Historical Global-Mean Surface Temperature Change in CMIP5 Models?

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Projections of long-term changes in solar radiation based on CMIP5 climate models and their influence on energy yields of photovoltaic systems

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(2015) Kate Marvel et al.   Nature Climate Change

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Simulation of the spatial distribution of mineral dust and its direct radiative forcing over Australia

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