Acetone is one of the most abundant oxygenated volatile organic compounds (VOCs) in the
atmosphere. The oceans impose a strong control on atmospheric acetone, yet the oceanic …

Current chemistry climate models do not include polar emissions and chemistry of halogens.
This work presents the first implementation of an interactive polar module into the very short …

We quantify the stratospheric injection of brominated very short‐lived substances (VSLS)
based on aircraft observations acquired in winter 2014 above the Tropical Western Pacific …

Water vapour convectively injected into the mid-latitude lowermost stratosphere could affect
stratospheric ozone. The associated potential ozone loss process requires low temperatures …

UCATS (the UAS Chromatograph for Atmospheric Trace Species) was designed and built
for observations of important atmospheric trace gases from unmanned aircraft systems …

Abstract Reactive halogens (X+ XO, X= I, Br or Cl) catalytically destroy a fraction of
tropospheric ozone under present‐day (PD) conditions, however, their distribution and …

The effectiveness of transport of short-lived halocarbons to the upper troposphere and lower
stratosphere remains an important uncertainty in quantifying the supply of ozone-depleting …

Snow and ice in Earth's cryosphere greatly affects the overlaying atmosphere. Sunlit natural
snowpack and ice surfaces may emit a wide range of trace gases, such as reactive nitrogen …