8th Workshop on Long-Term Changes and Trends in the Atmosphere;
Cambridge, United Kingdom, 28–31 July 2014
A new database seeks to improve estimates of oceanic emissions of methane and nitrous oxide.
An idealized climate model suggests polar warming stabilizes the jet stream and reduces atmospheric blocking at midlatitudes.
How can a complex atmospheric process be simplified for a model?
Airborne measurements put methane emissions from Colorado's Denver-Julesburg Basin at 12 to 26 tons per hour.
A new ice core measurements-based record of a climate-active gas shows variability on millennial timescales.
To climate scientists, marine fog's physical opacity symbolizes how much remains to be discovered about the atmospheric phenomenon.
Processes in the polar atmosphere can cause nitric oxide (NO)-enriched air to descend and destroy stratospheric ozone. Scientists explore one cause of these NO fluxes, stratospheric sudden warming.
Scientists projected that the upper atmosphere would continue to cool and contract with rising greenhouse gas emissions. Now, these projections have been confirmed for the first time.
Researchers explored how lunar gravity affects the density of the thermosphere. The study could help improve the accuracy of satellite orbit predictions.
