The phrase "atmospheric evolution" is correct and usable in written English.
It can be used in contexts discussing changes or developments in the atmosphere over time, often in scientific or environmental discussions.
Example: "The study of atmospheric evolution is crucial for understanding climate change and its impacts on our planet."
Alternatives: "atmospheric development" or "changes in the atmosphere".
They found two regimes of atmospheric evolution; the erosive regime and the accumulative regime.
The atmospheric evolution in their paper seems to have a more erosive history than that suggested by our results.
Numerous impact events during the heavy bombardment period would have the great consequences for the atmospheric evolution, especially for the atmospheric pressure change on the planets.
Finally we present an innovative new idea on how hydrogen clouds and energetic neutral atom (ENA) observations around transiting Earth-like exoplanets by space observatories such as the WSO-UV, can be used for validating the addressed atmospheric evolution studies.
Next, we present and analyse the atmospheric evolution to a steady state, the atmospheric circulation, the atmospheric temperature structure and the ozone volume mixing ration distribution (O3 V M R).
Finally we discuss in Section 6 a new innovative idea how one can test the atmospheric evolution theories addressed in Section 5 by transit observations of Earth-size exoplanets, which are exposed to higher SXR/EUV fluxes of dwarf stars.
Fig. 3 CTLE, WTLE and PDE atmospheric temporal evolution.
During atmospheric aging the evolution of size and composition of primary particles, i.e. particles that enter the atmosphere in the condensed phase, is influenced by condensation and evaporation of vapors.
The lidargram of course includes the effects of neutral atmosphere dynamics on the Na layer as these atoms have a long lifetime relative to the evolution of atmospheric dynamics and they are collisionally well-embedded in the atmosphere.
In this third decomposition step we assume the participation of atmospheric oxygen and gradual evolution of NOX.
Additionally, single-point CO2 measurements can be utilized as turbulence proxies and can give information on the evolution of atmospheric electricity properties (i.e., PG).
