Results 51 to 60 of about 103,038 (326)
Retrieving the age of air spectrum from tracers: principle and method [PDF]
Surface-emitted tracers with different dependencies on transit time (e.g., due to chemical loss or time-dependent boundary conditions) carry independent pieces of information on the age of air spectrum (the distribution of transit times from the surface).
A. Podglajen, F. Ploeger
doaj +1 more source
Tuning of a convective gravity wave source scheme based on HIRDLS observations [PDF]
Convection as one dominant source of atmospheric gravity waves (GWs) has been the focus of investigation over recent years. However, its spatial and temporal forcing scales are not well known.
Q. T. Trinh +7 more
doaj +1 more source
Ozone and Tracer Transport Variations in the Summer Northern Hemisphere Stratosphere [PDF]
Constituent observations from the Upper Atmosphere Research Satellite (UARS) in combination with estimates of the residual circulation are used to examine the transport and chemical budgets of HF, CH4 and O3 in the summer Northern Hemisphere.
Andrews +43 more
core +2 more sources
Transport Out of the Antarctic Polar Vortex from a Three-dimensional Transport Model [PDF]
[1] A three-dimensional chemical transport model is utilized to study the transport out of the Antarctic polar vortex during the southern hemisphere spring.
Bourke +42 more
core +4 more sources
How stratospheric are deep stratospheric intrusions? [PDF]
Abstract. Preliminary attempts of quantifying the stratospheric ozone contribution in the observations at the Zugspitze summit (2962 m a.s.l.) next to Garmisch-Partenkirchen in the German Alps had yielded an approximate doubling of the stratospheric fraction of the Zugspitze ozone during the time period 1978 and 2004.
T. Trickl +5 more
openaire +9 more sources
How robust are stratospheric age of air trends from different reanalyses? [PDF]
An accelerating Brewer–Dobson circulation (BDC) is a robust signal of climate change in model predictions but has been questioned by trace gas observations.
F. Ploeger +11 more
doaj +1 more source
The stratosphere is that part of the atmosphere which lies between ca. 10 and 50 km above the surface of the Earth and which contains the ozone layer. It is the seat of much interesting behaviour in terms of dynamics, radiation and chemistry, now revealed in detail by observations from modern space instruments, but still not completely understood ...
openaire +3 more sources
The potential role of stratospheric ozone in the stratosphere‐ionosphere coupling during stratospheric warmings [PDF]
The recent discovery of large ionospheric disturbances associated with sudden stratospheric warmings (SSW) has challenged the current understanding of mechanisms coupling the stratosphere and ionosphere. Non‐linear interaction of planetary waves and tides has been invoked as a primary mechanism for such coupling.
Goncharenko, Larisa +3 more
openaire +3 more sources
Beyond Earth: Resilience of Quasi‐2D Perovskite Solar Cells in Space
In the article (DOI: 10.1002/adma.202520433), Christoph Putz and co‐workers demonstrate rigid quasi‐2D perovskite solar cells operating in low Earth orbit, delivering stable power for more than 100 days under real‐space conditions. In‐orbit performance is correlated with extensive ground‐based thermal and proton‐irradiation studies on rigid and ...
Christoph Putz +17 more
wiley +1 more source
Stratospheric predictability and sudden stratospheric warming events [PDF]
A comparative study of the limit of predictability in the stratosphere and troposphere in a coupled general circulation model is carried out using the National Center for Environmental Prediction (NCEP) Climate Forecast System Interactive Ensemble (CFSIE).
Cristiana Stan, David M. Straus
openaire +1 more source

