First results of the Last Millennium Climate Reanalysis Project demonstrate the potential of the method to improve historical climate estimates by linking proxy data with climate models.
everything atmospheric
Storms Cause Infrequent Turbulence for Aircraft, New Study Finds
Scientists using lightning sensors to automate air-turbulence detection have found evidence that storms jostle aircraft much less than previously thought.
Pluto's Interactions with the Solar Wind Are Unique
Space physicists say that Pluto's atmosphere interacts with the solar wind in a never-before-seen hybrid way, one that's both comet-like and planet-like.
Four Perspectives on Order From Chaos
What makes thunderstorms clump, even to the point of singularity, over uniform oceans? Three recent papers in JAMES address this question, and a new Commentary ties them together.
Scientists Find Dead Lightning Branches That Come Back to Life
The detached bursts of brilliance might explain why the lowest point of a lightning bolt will sometimes suddenly brighten by up to 50% and double its speed as it hurtles to Earth.
New Approaches for Air-Sea Fluxes in the Southern Ocean
Air-Sea Fluxes for the Southern Ocean: Strategies and Requirements for Detecting Physical and Biogeochemical Exchanges; Frascati, Italy, 21–23 September 2015
Connecting Thunderstorms and Climate Through Ozone
New data links thunderstorms to climate via their impacts on aerosols, ozone, and water vapor in the stratosphere.
Ionospheric Waves Linked to Polar Atmospheric Dynamics
Ionospheric waves are likely to be caused by processes in the polar atmosphere rather than by space weather.
Blowin’ in the Wind: Observing Stratospheric Aerosols
New observations and understanding of stratospheric particles are crucial for evaluating their role in climate change.
A Decade of Progress in Stratospheric Aerosol Research
Enhanced technology and chemistry-climate models have advanced our understanding of the sources and processes controlling the evolution of the stratospheric aerosol layer, the so-called Junge layer.
