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Submitted:

• Brown, H. Y., McCoy, D. T., Nugent, J. M., Wang, H., Wu, M., Zhang, K., & Burrows, S. M. (2026). Sensitivity of anthropogenic cloud droplet number change to preindustrial emission inventories and physics parameterizations. ESS Open Archive. doi: 10.22541/essoar.176860194.44608635/v1 (Under review at GRL).

• Nugent, J. M., Brown, H., McCoy, D. T., Regayre, L.,Brown, H., McCoy, D. T., Regayre, L., Ghosh, K., Elsaesser, G. S., Bhatti, Y., Mülmentstädt, J., Song, C., Burrows, S. M., Watson-Parris, D., Grosvenor, D. P., Carslaw, K., Gettelman, A., & Eidhammer, T. (2026). Constraints on aerosol-cloud interactions from Earth system models suggest a warmer future. (Under review at Science)

Peer-reviewed:

• Jones, D. B., Brown, H. Y., Nugent, J. M., Mikkelsen, A., Song, C., Zhang, D., Burrows, S. M., Gordon, H., Kirby, A., & McCoy, D. T. (2026). Surface observations from Atmospheric Radiation Measurement sites constrain the anthropogenic contribution to cloud droplet number. Geophysical Research Letters, 53, e2025GL121383. doi: 10.1029/2025GL121383.

• Nugent, J. M., Brown, H., Kirby, A., McCoy, D. T., Allen, G., Aerenson, T., et al. (2026). Overview of the Nephele Perturbed Parameter Ensemble for aerosol-cloud interactions in E3SMv3. Journal of Advances in Modeling Earth Systems, 18, e2025MS004989. doi: 10.1029/2025MS004989.

• Aerenson, T., McCoy, D., Elsaesser, G., Wu, J., Nugent, J. M., Brown, H., Mikkelsen, A., & Zelinka, M. (2025). Global models predict clouds at the wrong time of day: does it matter for radiation and climate? Science Advances, 11, eady3236. doi: 10.1126/sciadv.ady3236.

• Wu, E., Rebassoo, F. O., Paul, P., Proistosescu, C., Nugent, J. M., McCoy, D. T., Caldwell, P. M., & Bretherton, C. S. (2025). Applying the ACE2 Emulator to SST Green’s Functions for the E3SMv3 Global Atmosphere Model. JGR: Machine Learning and Computation, 2, e2025JH000774. doi: 10.1029/2025JH000774.

• Nugent, J. M., Bretherton, C. S., & Blossey, P. N. (2025). What sets the tropical cold point in GSRMs during boreal winter? Overshooting convection vs. cirrus lofting. Earth and Space Science, 12, e2024EA003887. doi: 10.1029/2024EA003887

• Perkins, W. A., Brenowitz, N. D., Bretherton, C. S., & Nugent, J. M. (2024). Emulation of Cloud Microphysics in a Climate Model. Journal of Advances in Modeling Earth Systems, 16(4), e2023MS003851. doi: 10.1029/2023MS003851

• Nugent, J. M., & Bretherton, C. S. (2023). Tropical Convection Overshoots the Cold Point Tropopause Nearly as Often Over Warm Oceans as Over Land. Geophysical Research Letters, 50(21), e2023GL105083. doi: 10.1029/2023GL105083

• Nugent, J. M., Turbeville, S. M., Bretherton, C. S., Blossey, P. N., & Ackerman, T. P. (2022). Tropical cirrus in global storm-resolving models: 1. Role of deep convection. Earth and Space Science, 9, e2021EA001965. doi: 10.1029/2021EA001965.
• Turbeville, S. M., Nugent, J. M., Ackerman, T. P., Bretherton, C. S., & Blossey, P. N. (2022). Tropical cirrus in global storm-resolving models: 2. Cirrus life cycle and top-of-atmosphere radiative fluxes. Earth and Space Science, 9, e2021EA001978. doi: 10.1029/2021EA001978.