We provide observational evidence that energy release and aerosol emissions from rice-residue burning in northwestern India influence land surface temperature, with implications for the regional radiative budget. Multisatellite observations and reanalysis data are used to quantify land surface temperature responses to variability in aerosols and fire intensity. These responses display strong spatial heterogeneity, highlighting the interplay between fire, aerosol, and meteorological conditions.

Winds in the Equatorial region remain difficult to model. We take advantage of long-duration balloon campaigns from 2019 and 2021 to assess errors in winds between 18 and 20 km in a weather forecast model. Large errors persist: one third of the time, the error is larger than 3.5 m per second. This has implications for research studies that calculate air mass trajectories in this transition region between the troposphere and the stratosphere.

We assess the temperature, moisture, and dynamics in the upper troposphere-lower stratosphere simulated over South Asia in a high-resolution model relative to aircraft data. The lower stratosphere tends to be too warm, too dry, and too quiescent in the model, and as a result, too few ice clouds are predicted to form there. These biases could affect radiative balance and circulation in other areas also, as significant upward transport of moisture and pollutants occurs during the Asian monsoon.

Atmospheric particles over the ocean contain organic nitrogen, affecting climate and ecosystems. This first pole-to-pole study of marine air reveals a strong latitudinal divide, with higher concentrations in the polluted Northern Hemisphere. A key discovery is that air influenced by Antarctic sea ice is enriched in organic nitrogen, revealing a major natural source. Our new dataset improves climate models by clarifying how human emissions and natural processes shape the atmosphere.

Ubiquitous semi-volatile compounds can co-condense on aerosol particles with water vapour when relative humidity increases. Simulations of cloud formation at a boreal forest site with a cloud parcel model that accounts for non-ideal organic–inorganic interactions yield an enhancement of cloud droplet number concentration from co-condensing NH₃, HNO₃, and organics up to 44%, with strong sensitivities to volatility distributions, aerosol size distribution, and updraft velocity.

This study examined changes in the total ozone column above three Antarctic stations in 2007–2023 using ground and satellite observations. Ozone changes were mainly influenced by stratospheric temperature and atmospheric circulation. A significant increase occurred at Marambio, and unusually warm conditions in September 2019 caused ozone to rise strongly over East Antarctica, improving understanding of how the ozone layer responds to environmental changes.