npj Climate and Atmospheric Science

npj Climate and Atmospheric Science, Published online: 20 August 2026; doi:10.1038/s41612-026-01515-4 Monsoon–ocean competition shapes the record-low 2023 western North Pacific tropical cyclone season

npj Climate and Atmospheric Science, Published online: 20 August 2026; doi:10.1038/s41612-026-01510-9 Improvement of riming process parameterization in the WRF model and its advantages in simulating precipitation over the Tibetan Plateau

npj Climate and Atmospheric Science, Published online: 20 August 2026; doi:10.1038/s41612-026-01516-3 Impact of heterogeneous particle distributions on secondary ice production through the rime-splintering process in isolated convective clouds

npj Climate and Atmospheric Science, Published online: 20 August 2026; doi:10.1038/s41612-026-01518-1 Tracing vegetation stress from space: isoprene emissions capture the spatiotemporal footprint of El Niño

npj Climate and Atmospheric Science, Published online: 19 August 2026; doi:10.1038/s41612-026-01506-5 Contrasting impacts of Greenland and Antarctic meltwater on tropical circulation

npj Climate and Atmospheric Science, Published online: 18 August 2026; doi:10.1038/s41612-026-01502-9 Author Correction: Longwave radiation responses to cloud property perturbations in blackbody clouds should not be assumed to be negligible

npj Climate and Atmospheric Science, Published online: 18 August 2026; doi:10.1038/s41612-026-01509-2 Aerosol particle size modulates cloud droplet effective radius responses over land and ocean in South Asia

npj Climate and Atmospheric Science, Published online: 17 August 2026; doi:10.1038/s41612-026-01511-8 Efficient nitrogen management as a win-win strategy for air quality, health, and climate

npj Climate and Atmospheric Science, Published online: 15 August 2026; doi:10.1038/s41612-026-01514-5 High-temporal-resolution chemical characterization of PM 0.1 at a Mediterranean background site

npj Climate and Atmospheric Science, Published online: 15 August 2026; doi:10.1038/s41612-026-01512-7 Anthropogenic emissions mitigation weakens projected springtime dust intensification in Africa

npj Climate and Atmospheric Science, Published online: 15 August 2026; doi:10.1038/s41612-026-01513-6 Skillful and interpretable ENSO prediction via a glass-box dynamical-deep learning model

npj Climate and Atmospheric Science, Published online: 14 August 2026; doi:10.1038/s41612-026-01504-7 Europe’s extreme temperatures and rainfall in finer detail: strengths and limits of climate model downscaling

npj Climate and Atmospheric Science, Published online: 14 August 2026; doi:10.1038/s41612-026-01505-6 Contrasting seasonal roles of external forcing and internal variability in East Asian temperature

npj Climate and Atmospheric Science, Published online: 13 August 2026; doi:10.1038/s41612-026-01503-8 Thermodynamic insights into the molecular evolution of water-soluble organic matter in suburban PM 2.5

npj Climate and Atmospheric Science, Published online: 13 August 2026; doi:10.1038/s41612-026-01497-3 Multi-decadal evolution of ocean–monsoon teleconnections and the resurgence of ENSO influence on Indian summer monsoon rainfall

npj Climate and Atmospheric Science, Published online: 12 August 2026; doi:10.1038/s41612-026-01507-4 Synthetic UV filters: a previously unrecognized atmospheric heating agent

npj Climate and Atmospheric Science, Published online: 10 August 2026; doi:10.1038/s41612-026-01508-3 Topographic aspect shapes temperature lapse rates and land–atmosphere energy exchange in global mountains

npj Climate and Atmospheric Science, Published online: 07 August 2026; doi:10.1038/s41612-026-01496-4 Increasing synchronized hourly heavy rainfall over South China reflects enhanced multi-cluster and multi-regional coactivity

npj Climate and Atmospheric Science, Published online: 06 August 2026; doi:10.1038/s41612-026-01500-x Toward a deeper understanding of tropical cyclone precipitation: insights from SHAP-based AI attribution

npj Climate and Atmospheric Science, Published online: 05 August 2026; doi:10.1038/s41612-026-01498-2 Why does El Niño develop slowly but decay rapidly