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The Role of Atmospheric Composition in Defining the Habitable Zone Limits and Supporting E. coli Growth. [PDF]
Life (Basel)Kuzucan A +6 more
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Growth and Assemblage Dynamics of Temperate Forest Tree Species Match Physiological Resilience to Changes in Atmospheric Chemistry. [PDF]
Glob Chang BiolOulehle F +9 more
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Near-future rocket launches could slow ozone recovery. [PDF]
NPJ Clim Atmos SciRevell LE +9 more
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ExoFrontiers, 2021
Atmospheric gravity waves (GWs) are rather short in wavelength (1km – 100km in the horizontal, 100m – 10km in the vertical). Excited mostly below 10km altitude, through processes such as flow over mountains, thunderstorms, and other heavy weather, they ...
A. Showman
semanticscholar +2 more sources
Atmospheric gravity waves (GWs) are rather short in wavelength (1km – 100km in the horizontal, 100m – 10km in the vertical). Excited mostly below 10km altitude, through processes such as flow over mountains, thunderstorms, and other heavy weather, they ...
A. Showman
semanticscholar +2 more sources
Geophysical Research Letters, 2020
The atmospheric mechanisms responsible for the loess grain‐size variations in central Asia are less clear, and an increasing number of studies have found that the coarse‐grained component is likely supplied by the surface circulation rather than by the ...
Hao Lu +11 more
semanticscholar +1 more source
The atmospheric mechanisms responsible for the loess grain‐size variations in central Asia are less clear, and an increasing number of studies have found that the coarse‐grained component is likely supplied by the surface circulation rather than by the ...
Hao Lu +11 more
semanticscholar +1 more source
1996
The Earth’s atmosphere is an open system far from thermal equilibrium. It is irradiated by the shortwave radiation of the sun, emits radiation in the infrared and continuously exchanges matter, energy and momentum with the cryosphere, the hydrosphere, the biosphere and the lithosphere. Systems far form equilibrium can spontaneously form spatio-temporal
Gerd K. Hartmann +2 more
openaire +2 more sources
The Earth’s atmosphere is an open system far from thermal equilibrium. It is irradiated by the shortwave radiation of the sun, emits radiation in the infrared and continuously exchanges matter, energy and momentum with the cryosphere, the hydrosphere, the biosphere and the lithosphere. Systems far form equilibrium can spontaneously form spatio-temporal
Gerd K. Hartmann +2 more
openaire +2 more sources
Geophysical Research Letters, 2019
An efficient modeling strategy is proposed for the investigation of the effect of the sea surface temperature (SST) mesoscale variability on atmospheric dynamics.
Yinglai Jia +4 more
semanticscholar +1 more source
An efficient modeling strategy is proposed for the investigation of the effect of the sea surface temperature (SST) mesoscale variability on atmospheric dynamics.
Yinglai Jia +4 more
semanticscholar +1 more source