Results 171 to 180 of about 103,038 (326)
Cosmic ray-driven electron-induced reaction theory does not quantify spatiotemporal variations in lower-stratospheric ozone and temperature. [PDF]
Godin-Beekmann S +9 more
europepmc +1 more source
Transport to the Extratropical Stratosphere by Overshooting Storms in Idealized Simulations
Abstract Deep convection is a significant source of water to the extratropical stratosphere which can alter radiative properties and contribute to ozone loss. Previous studies find it responsible for 40% of mid‐latitude water vapor above 380K. However, the amount of hydration from individual storms and the mechanisms that initiate mixing is less ...
Devin P. Bissell +3 more
wiley +1 more source
Global stratospheric methane loss from satellite observations. [PDF]
Fu Q, Dong C.
europepmc +1 more source
Impact of Non‐Classical Gravity‐Wave Dynamics on Middle‐Atmosphere Mean Flow and Solar Tides
Abstract Conventional gravity‐wave (GW) parameterizations neglect three aspects of GW dynamics. Instead of momentum and entropy fluxes they use Eliassen‐Palm fluxes, thereby neglecting the possibility that resolved flow are not in geostrophic and hydrostatic balance.
T. Kühner, G. S. Völker, U. Achatz
wiley +1 more source
Projecting nitrous oxide over the 21st century, uncertainty related to stratospheric loss. [PDF]
Prather MJ, Wilson CP.
europepmc +1 more source
Stratospheric Aircraft: Impact on the Stratosphere?
The steady-state distribution of natural stratospheric ozone is primarily maintained through production by ultraviolet photolysis of molecular oxygen, destruction by a catalytic cycle involving nitrogen oxides (NO{sub x}), and relocation by air motions within the stratosphere.
openaire +1 more source
A Signal‐Derived Retrieval Reduces Bias in TEMPO NO2
Abstract Satellite measurements of NO2 ${\text{NO}}_{2}$ are widely used for investigations of emissions, pollution exposure, and photochemical ozone production. The most commonly available data products compromise on accuracy and spatial resolution in favor of lower compute time.
S. J. Beaudry, R. C. Cohen
wiley +1 more source
Stratospheric precursor induces wintertime phase reversal of the "warm Arctic-cold Eurasia" pattern. [PDF]
Zhang Y, Yin Z, Tian W, He S, Hsu P.
europepmc +1 more source

